Evaluation of Light Intensity and Soil Nutrients on the growth of Maize
Transcript of Evaluation of Light Intensity and Soil Nutrients on the growth of Maize
CHAPTER ONE
1.0 INTRODUCTION
1.1 Background of study
Maize (Zea mays L.) is a very important crop in the
tropics grown for a lot of purpose ranging from direct
consumption by man and animals to various industrial
uses (Powell et al., 2004). The production of maize in
Southern Nigeria has being in the decline for some
decades now (Eleweanya et al., 2005). Part of this decline
has been attributed to soil acidity problem in the area
(Pandey et al., 1994), which has reduced the soil pH to
less than 5.5 (Ahn, 1993).
Maize can be grown successfully on soils with a pH
of 5.0 – 7.0 but a moderately acid environment of pH
6.0 – 7.0 is optimum (Khanna and Raison, 2006). Outside1
the range results in nutrient deficiency and mineral
toxicity (Khanna and Raison, 2006). In order to
ameliorate this problem of soil acidity, ash is added
to the soil so as to reduce soil acidity, improve soil
fertility and also help the soil release certain
nutrients (Khanna and Raison, 2006). Some of these
nutrients include; Nitrogen (N), Phosphorus (P),
Calcium (Ca) and Magnesium (Mg). Maize can be grown on
a wide variety of soil, but perform best on well
drained, well aerated, deep warm loams and silt loams
containing adequate organic matter and well supplied
with available nutrients. Although it grows on a wide
range of soils, it does not yield well on poor sandy
soils except with heavy application of fertilizer and
on clay soils, it does not tolerate water-logging, it
2
can be killed if it stands in water for as long as two
days (Khanna and Raison, 2006).
Light is a visible form of electromagnetic wave.
It makes it possible for plants to grow and produce the
food we eat. Plants derive this energy from sunlight by
means of photosynthesis. The characteristics of light
such as intensity, quality (color) and duration
determine to some extent the level of its interaction
with matter. Intensity of incoming radiation from the
sun is altered by both atmospheric and terrestrial
obstruction. A host of researchers (Ballare et al., 1991,
Baraldi et al., 1994 and Grantani, 1997) have shown that
change in spectral energy distribution affect plant
growth and development. Photoreceptors in plants are
divided into two: phytochrome principally sensitive to
3
light in the red and far-red regions of the visible
spectrum (Batschaver et al.,1998; Ballare, 1999 and Smith,
2000) and crytochrome and phototropin sensitive to blue
light (Briggs and Huala, 1999). Most plants use the
photoreceptors to regulate the time of flowering,
germination of seeds, elongation of seedlings, size and
shape of leaves, number of leaves, the synthesis of
chlorophyll and stomata opening (Gay and Hurd, 1975;
James and Bell, 2000; Henning, 2001 and Answer, 2006).
Photosynthesis is the process by which green
plants and certain other organisms (seaweeds, algae and
certain bacteria) use the energy of light to convert
carbon dioxide and water into simple sugar (Leal,
2007). Light energy causes the electrons in chlorophyll
and light-trapping pigments to boost up the electrons
4
only out of their orbits, the electrons instantly fall
back into place releasing vibration energy as they go,
all in millionths of a second. Chlorophyll and the
other pigments absorb the energy released by the
electrons which is used during photosynthesis. Plants
from different environments have different responses to
colors of light. Branching, internodes length and
flowering initiation can all be affected by varying
degrees by the ratio of red light to far-red.
Therefore, it can be clearly seen from existing
literatures that light affects almost all processes
associated with growth, photosynthesis and flowering in
plants. The optimum temperature for plant growth and
development ranges from 30oC – 34oC. The cool
conditions at high altitude lengthen the cycle or
5
growing period. Temperatures below 5oC and above 45oC
results in poor growth and death of maize plant.
1.2 Objectives of study
This experiment aim at investigating the growth
performance of maize on different soil types treated
with plant ash and subjected to different light
intensity.
6
CHAPTER TWO
2.0 LITERATURE REVIEW
2.1 Taxonomy
Maize is the most important cereal in the world
after wheat and rice. It is unique among cereals. The
grains are borne in separate inflorescence, which are
completely enclosed as modified leaf sheaths or husk,
7
so that it is incapable of dispersing its sheets. The
genus Zea belongs to the tribe Andropogoneae in the
subfamily Panicoidea in the family Poaceae (Reviewed in
OECD, 2003 and USDA, 2005). There are currently eighty-
six (86) recognized genera within the Andropogoneae
tribe (USDA, 2005). Currently, there are five species
included in the genus Zea. Species of Zea that have been
examined, largely have a chromosome number of 2n = 20,
except for Z. perennis (perennial teosinte with 2n =
40) (as reviewed in Ellneskog-Staam et al., 2007). The
species Z. nicaraguensis was described by Bennett et al.
(2003), it is closely related to Z. Luxurians but
currently, the number of chromosomes and sexual
compatibility with other Zea spp are unknown.
8
2.2 Morphology
2.2.1 Plant morphology
The typical maize plant is a tall (1-4m) annual
grass (monocot) which forms a seasonal root system
bearing a single erect stem (culm) made up of nodes and
internodes, although some cultivars may develop
elongated lateral branches (tillers). Many temperate
cultivars are shorter than tropical (and subtropical)
cultivars. Nodes gradually taper to the top of the
plant. Leaves are broad and a single leaf develops at
each node in two opposite ranks, the leaf arrangement
is distichous (reviewed in Esau, 1977). Each leaf
consists of a sheath surrounding the stalk and an
expanded blade connected to the sheath by the blade
joint. The mature plant can have up to approximately
9
thirty leaves, with considerable variation in leaf
number, size and orientation between maize races.
Generally, tropical maize plants develop more leaves
than temperate cultivars. Maize, like many plants that
evolved under tropical conditions is a C4 (that is,
Hatch and Slack cycle) plant and therefore, more
efficient at utilizing carbon dioxide than C3 (Calvin
cycle) plants. The physiological characteristics are
reflected in leaf morphology down to the microscopic
level. For example, bundle sheath cells are richer in
chloroplasts than mesophyll cells. The chloroplasts are
also larger than those of mesophyll cells (Reviewed in
Esau, 1977).
2.2.2 Reproduction morphology
10
Maize is a monoecious plant: one or more lateral
branches, the shanks develop in the leaf axis of the
plant. They terminate in a female inflorescence, an
ear. The male inflorescence, the tassel, forms at the
top of the stem. Usually one or two lateral shoots in
the upper part of the plant develop into female
inflorescences. The shank consists of nodes and short
internodes, the lengths of which vary between maize
races. The ear is covered in a number of leaves called
husks. Those leaves differ in appearance when compared
to those on the stalk; they surround and protect the
developing ear. Where maize is left to dry in the
fields, more husks are generally desired to protect the
grains from birds and insects. Where maize is harvested
earlier, it is often desirable for a cultivar to have a
lower number of thin husks. The ear does not usually11
show any lateral branching. The thick axis of the ear
the cob, bears an even number of rows of ovaries, each
containing a single ovule .The number of ovules that
will develop into kernels ranges from three hundred to
one thousand and is dependent on the cultivar/variety
as well as factors occurring later in development
(Purseglove, 1972). The silks of the maize ear are the
stylar canals of the mature ovaries.
2.3 Forms of maize
A number of maize can be described on the basis of
endosperm and kernel composition (Paliwal, 2000 and
Darrah et al., 2003).
1. Flint maize: Flint maize kernels are
characterised by their high percentage of hard
endosperm around a small soft centre.
12
2. Dent maize: It is the most commonly grown for
grain and silage, and is the predominant type grown in
the U.S.A. Hard endosperm is present on the sides and
base of the kernel. The remainder of the kernel is
filled with soft starch, when the grain starts drying
the soft starch at the top of the kernel contracts,
producing the depression for which it is named.
3. Floury maize: Is being grown predominantly in the
Andean region. Its endosperm is mainly composed of soft
starch, making it easy to grind and process into foods.
4. Waxy maize: Waxy maize kernels contain almost
entirely amylopectin as their starch (rather than the
normal 70% amylopectin and 30% amylose). Waxy maize is
preferred for food in some part of East Asia and for
some industrial uses.
13
5. Pop maize: Pop maize kernels are characterised
by a high proportion of hard endosperm, which is much
higher than any other maize kernel. Pop maize is grown
on a small scale compared to other types but popped
kernels are consumed worldwide as a snack food
(Reviewed in Ziegler, 2003).
6. Sweet maize: Is grown for green ears (sweet
corn). The ears are harvested at approximately eighteen
to twenty days post pollinated when kernel moisture is
approximately seventy percent (70%). The developing
grain of sweet maize is higher in sugar content due to
one or more recessive mutations blocking conversion of
sugar starch.
7. Baby maize: The unfertilized young ear obtained
from sweet maize or other forms of maize is called baby
14
maize. This is rich in minerals and vitamins and can be
harvested within forty-five to fifty days after sowing
for marketing.
2.4 Reproduction
2.4.1 Asexual reproduction: Under natural condition
maize reproduces only through seeds
2.4.2 Sexual reproduction
Maize is a quantitative short-day plant but some
cultivars have low or no sensitivity to day-length
(Kiniry et al., 1983). In those cultivars that are
photoperiod sensitive, flowering may be delayed when
the photoperiod is greater than a critical threshold
15
value ranging from 10 – 13.5h (Kiniry et al., 1983). Those
adapted to the tropics may show delayed maturity if
grown in more temperate areas with longer days (Birch
et al., 2003). Initially male and female inflorescences
have primordia of bisexual flowers. However, during
their development, primordia of stamens abort in the
axillary inflorescences, the primordia of gynoecia
abort in the apical inflorescence. The apical meristem
elongates once the leaf premordia are initiated. It is
transformed into a reproductive meristem that develops
into the tassel. Pollen is shed from the tassel
continuously for a week or more as upper and lower
florets in the male spikelets show developmental
differences and the spikes mature asynchronously. The
female inflorescences (ears) arise from axillary buds
and bear flowers in rows along the cob. Development of16
the flowers and the ovules on the ear proceeds from the
base upwards (acropetal). From each flower a style
begins to elongate towards the tip of the cob, forming
long threads, or silks. Silk development begins from
the flowers near the base of the ear and proceeds
towards the tip over several days. Receptive silk
emerge over the husks over a period of three to five
days and can grow to more than 30.5cm length, extending
beyond the end of the husks. The silks have short
hairs, trichomes, which form an angle to the stylar
canals and help harboring pollen grains. Receptive
silks are moist and sticky. Maize is often considered
as protandrous (anthers reaching maturity before he
gynoecium), as anthers on the spikelets on the upper of
the central spike protrude out of the florets and start
shedding pollen one or two days (under optimal growth17
conditions) before the silk emerge above the husks.
However, the gynoecium matures and the silks become
receptive before they appear above the husk tips. Under
any stress (especially water stress), the interval
between pollen release and silk emergence increases.
2.5 Abiotic interactions
Maize plant shows wide genetic base for abiotic
stress tolerance, which is mirrored by its ability to
grow in a variety of environments. Although, it is
essentially a crop of warm climates with adequate
moisture (Purseglove, 1972) and is therefore not suited
to semi-arid or wet tropical climates. It is argued
that genetic improvement in maize yield over the past
seventy years is the result of changes to physiological
attributes that, in turn, have imparted enhanced
18
abiotic stress tolerance (Lee and Tollenaar, 2007) that
is, selection of hybrids for high density planting has
been accompanied by increased resistance to stresses
like drought and has permitted consistent performance
across a range of variable environments (Dhugga, 2007).
One way that abiotic stress affects the maize plant is
by moving the source-sink balance (Lee and Tollenaar,
2007). Classic symptoms of excess source capacity are
purpling of leaves, sheath tissues and stalks during
grain-filling while symptoms of excess sink capacity
are premature senescence of leaves and stalks during
grain-filling (Lee and Tollenaar, 2007).
2.5.1 Nutrient requirements
Maize grown commercially, whether for grain or
silage, has a high demand for nutrients, especially
19
Nitrogen (N), Phosphorus (P) and Potassium (K) (Birch
et al., 2003). In maize-growing areas of the tropics,
acids soils are widespread and plant growth is
constrained by the associated Aluminum toxicities that
lead to stunting and impairment of root growth and
subsequent inability of plants to take up moisture from
the soil (Lafitte, 2000).
2.5.2 Temperature requirements and tolerances
Maize is a summer-growing crop requiring warm day
time temperatures of between 250C – 300C and cool
nights (Colless, 1992). Temperature below 80C (or 00C
after silking) or above approximately 400C usually
cause cessation of development (Birch et al., 2003).
Different maize cultivars have different optimal
temperature requirements and, for example, tropical
20
cultivars derived from highland maize are better able
to grow and develop at lower temperatures than those
adapted to ‘lowland’ or ‘mid-altitude’ areas.
Temperatures that are outside the range of adaptation
of a cultivar may impact negatively on factors such as
photosynthesis, translocation and pollen viability. In
particular, high temperatures have negative impact on
the kernel growth, kernel mass and protein accumulation
(Monjardino et al., 2006).
Table 2.1Effects of temperature on key processes inmaize
Temperature Process EffectHightemperature
Photosynthesis Reduced above 400C due tomembrane damage,irreversible damage above
21
45oCRoot hormoneproduction(Abscisic acidand cytokinin)
Reduced hormone productionrestricts chloroplastdevelopment andphotosynthetic activity
Pollination Pollen viability reducedabove 350C especially ifthere is low humidity
Grain yield Grainfilling duration isreduced, grainfilling rateis increased. Overallyield is reduced.Exacerbated by waterstress
Lowtemperature
Photosynthesis Reduced due to reducedenzyme function andmembrane damage
Leaf extension Reduced due to reducedenzymes function andmembrane damage
Water andnutrientuptake
Reduced due to reducedenzyme function andmembrane damage in roots.
Grain yield Reduced, especially intropical lowland cultivarsat less than 150C.
Translocation Reduced, especially intropical lowland cultivarsat less than 100C
Source: Lafitte(2000).
22
2.5.3 Water
2.5.3.1 Water deficiency
Worldwide, the average yield losses in maize crops
due to drought can be high, particularly in the tropics
(Srinivasan et al., 2004). Rainfall is a limiting factor
for dry-land production of commercial maize crops and
irrigation is essential in areas with a winter dominant
rainfall pattern or where the amount of summer dominant
rain is high variable (Birch et al., 2003). Maize is
particularly susceptible to water stress at the
flowering stage when yield potential is being set23
(Srinivasan et al., 2004) especially as this coincides
with high evapotranspiration rates.
2.5.3.2 Water-logging
Significant annual losses in maize production can
occur because of water-logging (Srinivasan et al., 2004).
Plants growing for prolonged periods in waterlogged
soils show stomatal closure, reduced leaf area growth,
chlorosis, reduced root growth, root death and
ultimately plant mortality (Srinivasan et al., 2004).
Damage to roots is due mainly to the accumulation of
toxic products (such as lactic acid) as a result of
anaerobic respiration. Tropical and subtropical
cultivars are most susceptible to water-logging at the
early vegetative stage and at “knee high” stage
(Srinivasan et al., 2004). Molecular and cellular changes
24
to maize seedlings under short-term water-logging has
been widely studied as maize typically shows an
anaerobic “response” in which some twenty proteins,
mostly associated with glycolysis or sugar-phosphate
metabolism, are synthesized (Subbaiah and Sachs, 2003).
Root porosity, that facilitates oxygen diffusion from
the above ground parts to the submerged roots, is
increased by the selective death of root cortical cells
and helps to prolong the survival of plants (Subbaiah
and Sachs, 2003). Root tip death, also characteristic
of response to anoxia, may enhance survival and
subsequent recovery, when water-logging is removed by
eliminating an area of metabolically active tissue
(Subbaiah and Sach, 2003). Development of adventitious
root on the soil surface is also important in
conferring flooding tolerance (mano et al., 2005).25
2.6 Biotic interaction
2.6.1 Weeds
Although, maize is a vigorous and tall growing
plant, it is susceptible to competition from weeds,
particularly at the early stages of growth (Morris,
2008). Weeds may directly lead to yield reduction by
competing with the maize plant for nutrients and water
(James et al., 2000). Weed management can take a number of
forms with an integrated approach being recommended
(Farell and O’Keeffee, 2007) and including crop
rotations, planting into weed-free seedbeds, pre-plant
cultivation, use of pre-plant/pre-emergence/post-
emergence herbicides (O’Gara, 2007). A range of
herbicides offer flexible options for weed control and
often two herbicides can be used in combination to give
26
a broader spectrum of control (O’Gara, 2007). Commonly
used herbicides include atrazine, flumetulan, dicamba,
metolachlor, fluroxypyr, propachlor, pendimethalin,
tribenuronmethyl and triclopyr (Storrie et al., 2005).
2.6.2 Insects
Maize is most susceptible to damage by insects
during the establishment phase when soil insects can
cause up to 30% losses and necessitate replanting of
the crop, and from tasselling to harvest (O’Gara,
2007). Invertebrate pest establishing crops damage
germinating seeds and seedlings and include black field
earwigs, wireworms, false wireworm, cutworms, maize
stem borer, and beetles such as African black beetle.
The recent development of insecticidal seed treatments
(examples, imidicloroprid and thiamethoxam) has help to
27
control soil pests and some above ground insects
(O’Gara, 2007).While more traditional methods such as
in-furrow spraying and agronomic practices at sowing
are also effective (Hughes, 2006).
2.7 Nutritional components of maize kernel
The typical mature kernel as a whole is composed
of 70-75% starch, 8-10% protein and 4-5% oil (Boyer and
Hannah, 1994). However, there are large differences in
the relative concentrations of these components between
different parts of the kernel. The two major structures
of the kernels are the endosperm and the germ (embryo),
constituting about 80% and 10% of the mature kernel dry
weight, respectively. The endosperm is largely starch
(approximately 90%) while the germ contains high levels
28
of fat (approximately 33%) and protein (approximately
18%).
Table 2.2 Relative content (%) of nutrient componentsin parts of the maize kernel
Nutrient Pericarp/Seedcoat
Endosperm Germ(embryo)
Protein 3.7 8.0 184Crude fibre 86.7 2.7 8.8Crude fat 1.0 0.8 33.2Starch 7.3 87.6 8.3Sugar 0.34 0.62 10.8
Source: FAO(1992).
2.8 Beneficial phytochemicals
Maize is considered an important food crop for
humans and a high-energy feed for animals (FAO, 1992).
In humans diet it is a good source of vitamin B1, B5,
29
folate, dietary fibre, vitamin C, phosphorus and
manganese and as a staple food it compares favourably
with root and tuber crops and is similar in energy to
dried legumes (Okuruwa and Kling, 1996). The average
nutritional content of various forms of maize is given
in Table 2.2; processing reduces the concentration of
proteins, lipids and fibres (FAO, 1992).
Table 2.3Ranges for proximate analysis of maize grain,sweet corn kernels and silage
Maizegrain
Sweetcorn
Maizesilage
Moisture % freshweight
7-23 74.7-84 62-78
Protein % dryweight
6-12 11.3-15.6 4.7-9.2
Lipid % dryweight
3.1-5.8 4.86-8.75
Ash % dryweight
1.1 – 3.9 2.58-3.86 2.9-5.7
Carbohydrate
% dryweight
82.2-82.9 72.5-79.18
Fibre % dryweight
8.3-11.9 11.2-15.6 40-48.2
30
Source: OECD (2002).
2.9 Commercial uses
Maize is one of the oldest cultivated grains and
one of the most productive crop species with a global
average yield of more than four tonnes per hectares
(Reviewed in Paliwal, 2000 and Farnham et al., 2003). It
can be directly consumed as food at various
developmental stages from baby corn to mature grain. A
high proportion of maize produced is used as stock
feed, for example, 40% in tropical areas and up to 85%
in developed countries (Reviewed in Paliwal, 2000 and
Farnham et al., 2003). It can be fed to stock as green
31
chop, dry forage, silage or grain. Various fractions of
milling processes can also be used as animal feed.
Stover is the term used to describe the dried stalks
and leaves of a crop used as animal fodder after the
grain has been harvested. Maize can be processed for a
range of uses both as an ingredient in food or drink,
for example corn syrup in soft drinks or maize meal or
industrial purposes. Maize is the major source of
starch worldwide and is used as a food ingredient,
either in its native form or chemically modified
(White, 1994). Maize starch can be fermented into
alcohol, including fuel ethanol, while the paper
industry is the biggest non-food user of maize starch.
The oil and protein are often of commercial value as
by-products of starch production and are used in food
32
manufacturing (Boyer and Hannah, 1994; Paliwal, 2000;
Hobbs, 2003 and McCutcheon, 2007).
2.10 Effects of light on plant growth and development
Light is made up of energy. Light to plants is the
wavelengths of the electromagnetic spectrum. Light for
plant is used for producing food through the process of
photosynthesis (Bjorn, 1994). The characteristics of
direction and spectral composition of light in the
plants environment is transferred to the plant through
the interception and activation of pigment systems
within the leaf. Plants also use light for sensing and
detecting competitors and keeping track of time (Bjorn,
1994).
2.10.1 Light quality
33
Sunlight is often referred to as white light and
is composed of all colors of light (Bjorn, 1994). A
color of light would be the relative distribution of
wavelengths from a radiation or reflective source.
2.10.2 Light intensity
Light intensity is a major factor governing the
rate of photosynthesis. The quantity or amount of light
received by plants in a particular region is affected
by the intensity of the incident (incoming) light and
the length of the day (Bjorn, 1994).The intensity of
light changes with elevation and latitude. The amount
of sunlight also varies with the season of the year and
time of day, as well as other factors, such as clouds,
dust, smoke or fog. Plants have varying preferences for
light intensity. The light saturation point of the
34
plant determines the relative light requirement of
plant (Bjorn, 1994). The light saturation point is the
point above which an increase in light intensity does
not result in an increase in photosynthetic rate. Crops
such as maize etc. require a relatively high level of
light for proper plant growth (Bjorn, 1994).
2.10.3 Light duration
Due to the tilt of the earth’s axis (23oC from
vertical, that is,
the inclination angle of a planets rotational axis in
relation to its orbital plane) and its travel around
the sun, the length of light period (also called
photoperiod or day-length) varies according to the
season of the year and latitude. It varies from a
nearly uniform twelve-hour (12h) day at the equator (O
35
latitude) to continuous light or darkness throughout
the twenty-four hours (24hrs) for a plant of the year
at the poles (Bjorn, 1994). Some plants change their
growth in response to day-length and exhibit
photoperiodism. One important plant response to day-
length in some plants is flowering. Some plants flower
when a specific day-length minimum has been passed.
Short day plants flower rapidly when the days get
shorter and long day plants flower fast when days get
longer. Plants that are not affected by day-length are
called neutral plants. These plants can flower under
any light period (Bjorn, 1994).
2.10.4 Light energy captured by plants
(Photosynthesis)
36
One of the main roles of light in the life of
plants is to serve as an energy source through the
process of photosynthesis using water and carbon
dioxide, through photosynthesis; plants produce the
foodstuff (photosynthate) necessary for growth and
survival. Subsequently, carbohydrates (starch and
sugar) and stored chemical energy are produced during
biochemical processes in plants (Bjorn, 1994). Plants
capture the energy in light using a green pigment
called chlorophyll. A very precise number of photons at
specific wavelengths (near 680nm) are required to split
a water molecule (H2O) within the green leaf, which
releases oxygen (O2) and provides chemical energy to
continue the long biochemical process to produce more
complex molecules such as carbohydrates. Carbon dioxide
37
from the air and water from within the leaf combine to
produce oxygen and photosynthates (Bjorn, 1994).
2.10.5 Light regulated plant development (Photo-
morphogenesis)
Photo-morphogenesis is defined as the ability of
light to regulate plant growth and development,
independent of photosynthesis. Plant process that
appear to be photomorphogenic include internode
elongation, chlorophyll development, flowering,
abscission, lateral bud outgrowth and root and shoot
growth (Bjorn, 1994). Photo-morphogenesis differs from
photosynthesis in several major ways. The plant pigment
responsible for light-regulated growth response is
phytochrome. Phytochrome is a colorless pigment that is
in plants in very small amounts. Only the red (600 to
38
660nm) and far red (700 to 740nm) wavelengths of the
electromagnetic spectrum appear to be important in the
light-regulated growth of plants. The wavelengths
involved in generating photosynthesis are generally-
broader (400 to 700nm) and less specific. Photo-
morphogenesis is considered a low energy response
(meaning that it requires very little light energy to
get a growth-regulating response). Plant generally
require greater amount of energy for photosynthesis to
occur (Bjorn, 1994).
CHAPTER THREE
3.0 MATERIALS AND METHODS
39
3.1 Study site
The experiment was carried out in 2013, from the
11th of June to the 19th of August at the Botanical
garden behind the Department of Microbiology site II,
Delta State University, Abraka, Delta State. Abraka
lies between Latitude 5O45’ and 5O50’ North of the
Equator and Longitude 6O and 6O15’ East of the
Greenwich meridian (Efe, 1994). Abraka falls between
the equatorial climate belt of Nigeria with mean
temperature of 30OC, the area is characterised by a
total annual rainfall of three hundred and ninety-eight
millimeters (398mm) with mean annual rainfall ranging
from two hundred and eighty-eight millimeters (288mm)
in December to six hundred and twenty eight point nine
millimeters (628.9mm) in September (Efe, 2006).
40
3.2 Sample collection
3.2.1 Source of seeds
The maize variety; composite maize was purchased
from Agricultural Development Programme (A.D.P.)
Effurun, Delta State, Nigeria.
3.2.2 Source of soil sample
Sandy soil was obtained from Abraka River (Ken-
dive) at Abraka, Ethiope-East Local Government Area of
Delta State, Nigeria. The other soil samples (loamy,
laterite and clay) were collected from a virgin land
from site III, Delta State University, Abraka, Delta
State, Nigeria.
3.2.3 Source of plant ash
41
Fresh grasses were cut at a site behind
Microbiology laboratory, site II, Delta State
University, Abraka, Delta State, Nigeria, they were
dried under natural condition and later burnt.
3.3 Experimental design
Randomized Complete Block Design (RCBD) with three
replications was used for the experiment.
3.4 Procedure
Five kilograms (5kg) of each of the soil samples
(loamy, sandy, laterite and clay) were measured and
filled into the polythene bags (37 × 33cm in dimension)
with a total of thirty-six polythene bags and they were
perforated to allow easy drainage of water. Seeds were
planted at a depth of 2cm into each of the polythene
bags and watered immediately and afterwards, every42
other day at 200ml. The experiment was replicated three
times and arranged in Randomized Complete Block Design
(RCBD) into the net that is, triple net (5 × 3 ft) and
the no-net and control were left outside. 5.56g of
plant ash was measured with an electronic compact scale
(g) and added to the plant one week after planting and
the setup was monitored for ten weeks and parameters
were measured. Germination count was taken per
polythene bag at seven days after sowing, when
germination commenced at day three after exposure to
sunlight for loamy, sandy and laterite while for clay
germination commenced at the 4th day after sowing.
Germination percentage was calculated, thus
% Germination =NumberofseedsgerminatedNumberofseedssown× 100
1
43
This procedure follows that of Edema and Etioyibo,
(2009). Seeds which failed to sprout within the seven
days period were regarded dead.
The growth parameters, leaf area, stem diameter
(girth) and leaf number were determined every two
weeks, the plant height were determined weekly while
sunlight intensity was taken daily. The light intensity
of the plant was determined using a light meter. Plant
height was determined using a meter rule; it was
measured from the soil level to the tip of the youngest
leaf. The leaf area determination was done by measuring
the length and breadth of the leaf and correction
factor of 0.75 was used to multiply the length and
breadth measurement following the procedure of Edema
and Etioyibo, (2009). The girth of the plant was
44
determined using a digital caliper. The number of
leaves was determined by visually counting the number
of leaves per polythene bag. For the dry weight
accumulation, the plants were harvested. These plants
were weighed (fresh weight) and oven dried at 55OC for
88hours following the procedure of Edema and Etioyibo,
(2009).
3.5 Statistical analysis
Data collected were analysed statistically using
One-way Analysis of Variance (ANOVA) and the
significant means were separated with the Duncan
multiple range test using the statistical analytical
system (SAS, 2005).
3.6 Chlorophyll analysis
45
The leaf chlorophyll content was estimated
according to the method of Zhang and Qu (2003). Ten
weeks after planting, the third or fourth leaf from the
apex of the plant from each polythene bag was
harvested, wrapped in a foil paper labeled and put in a
dark polythene bag. A weight of 0.10g of leaf tissues
were taken from each leaf sample and put in a 50ml
labeled McCartney bottles. Twenty millitres (20ml) of
eighty percent (80%) acetone was poured into each
McCartney bottle for the purpose of chlorophyll
extraction. The bottles were transferred to a dark
chamber and left to stand for twenty-four hours. After
extraction, the extracts were read for absorbance at
663 and 645nm wavelength in a spectrophotometer.
46
Chlorophyll content was calculated according to
the following formula:
Chla (mg/g) = 12.2A663−0.86A645XV
aX1000XW
Chlb (mg/g) = (19.3A645 -3.6A663)× Va × 1000 × W
Where a = Length of light path = 1cm
W = Fresh weight of leaf sample
V = Volume of solution
The result is expressed in mg/g FW (fresh weight).
3.7 Physicochemical analysis of soil and plant ash
47
3.7.1 pH: It is a measure of the negative logarithm
of the hydrogen ion concentration present in the
samples.
Apparatus: pH meter, 50ml beaker, 2mm sieve, wash
bottle, weighing balance and glass rod.
Reagent: Distilled water
Procedure
The soil sample was air-dried, grinded and sieved
with a 2mm sieve. Ten grams (10g) of the sieved soil
was weighed into a 50ml beaker. 25ml of distilled water
was added to the soil sample. It was allowed to settle
for thirty minutes, during this period the pH meter was
standardized with a buffer 4, 7 and 9. After thirty
minutes had elapsed, the soil sample in the beaker was
stirred with a glass rod and the pH meter electrode was48
immersed into the mixture. The pH of the solution was
noted (Ibitoye, 2006).
3.7.2 Organic carbon/Organic matter (wet oxidation)
Apparatus: 250ml conical flask, retort stand,
burette, measuring cylinder, 0.5mm sieve, mortar and
pistol.
Reagents:0.1MK2Cr2O7, 0.5M(NH4)2Fe(SO4)6H2O,
Diphenylamine indicator and concentrated sulphuric
acid.
Procedure
The soil sample was grinded to a fine powder. One
gram (1g) of the grinded soil sample was weighed into a49
250ml conical flask and 100ml of 0.1MK2Cr2O7was added.
20ml of H2SO4 was added rapidly and the flask swirled
vigorously for one minute immediately after the
addition of the concentrated acid. Thereafter the
solution was allowed to stand for thirty minutes. 100ml
of distilled water, followed by two drops of
diphenylamine indicator was added. The solution was
titrated against 0.5M (NH4)2Fe(SO4)6H2O in the burette
to a dark greenish end point. A blank titration was
also carried out.
Calculations
% Organic carbon = (B−T )×M×0.003×F×100W
% Organic matter = % organic carbon × 1.724
Where:
50
B = Blank titre value
M = Molarity of (NH4)2Fe(SO4)6H2O used
T = Titre value of sample
F = Correction factor = 1.33
W = Weight of sample = 1g
(Ibitoye, 2006).
3.7.3 Exchangeable bases (Ca, Mg, Na and K)
Apparatus: 250ml conical flask, beaker, burette,
retort stand, electronic shaker, shaking container,
flame photometer.
Reagents:0.2M EDTA, 1MNH4OAC, concentrated ammonia
solution, 2% KCN, 20% KOH, Erichrome black T and
meroxide indicators.
51
Procedure
Five grams (5g) of two millimeters sieved air-
dried soil was weighed into a shaking container, 50ml
of NH4OAC was added. The mixture was shaked in an
electrical shaker for one hour. The mixture was
filtered with a filter paper into a 100ml beaker flask,
10ml of the filtrate was pipetted into a 250ml conical
flask and 50ml of distilled water was added. Thereafter
12.5ml of concentrated ammonia solution and 1ml of 2%
KCN was added. This was followed by three drops of
Erichrome Black T indicator. The solution was titrated
against 0.02M EDTA in the burette to a blue end point.
52
The amount of Ca or Mg present in the soil sample was
computed by using the formula.
Ca or Mg (mMol/100g) = T × M × V1 × 100
V2W
Where;
T = Titre value of the sample
M = Molarity of EDTA used = 0.82M
V1 = Volume of extractant used = 50ml
V2 = Volume of extract used = 10ml
W = Weight of sample = 5g
While Na and K were determined by using a flame
photometer (Udo and Oginwale, 1996).
3.7.4 Nitrogen (N)
53
Procedure
Two grams (2g) of the soil was weighed into a
500ml macro, kjeldahl flask, 20ml of concentrated H2SO4
with one gram of catalyst mixture per sample. The
content was heated on a digestion stand until the
solution becomes clear and soil residue remaining
becomes white. It was heated further for few minutes to
ensure complete digestion. The solution was allowed to
cool and 50ml of distilled water was added, and
filtered into 100ml and made up to a mark-standard was
also prepared before reading with a spectrophotometer
(Esu, 1999).
54
3.7.5 Phosphorus (P) (Bray P-1)
Procedure
Five grams (5g) of the soil which has passed
through two millimeter sieve was weighed into a shaking
bottle, 35ml of extracting solution was added, it was
shaked for one minute and filtered into 250ml conical
flask. Phosphorus (P) was determined calorimetrically,
using spectrophotometer (Obi, 1990).
3.7.6 Exchangeable acidity (H+ and Al)
Five grams (5g) of the soil sample which has
passed through 2mm sieve was weighed into a shaking
bottle, 50ml of extracting solution (KCl) was added, it
was shaked for one hour and filtered into 250ml conical
flask. 200ml of the extract was pipetted into 250ml
conical flask, 100ml of distilled water followed by two55
drops of indicator (phenolphthalein) to a pink color
end point. For Al, it was back titrated using the
formula.
H+ or Al = T × M × V1 ×100
W × V2
Where:
T = Titre value of the sample
M = Molarity of EDTA used = 0.82M
V1 = Volume of extractant used = 50ml
V2 = Volume of extract used = 10ml
W = Weight of sample = 5g
(Ibitoye, 2006).
3.7.7 Particle size analysis (PSA)
Procedure56
Fifty grams (50g) of the soil sample after
passing through 2mm sieve was weighed into a shaking
container, 50ml of sodium hetamaphosphate (calgon) was
added and shake with an electrical shaker for thirty
minutes, after which it was transferred into a 1000ml
measuring cylinder and made up to a mark. It was then
inverted several times and the hydrometer was inserted
and the reading was taken after 40seconds that of the
temperature and blank was also taken, after two hours
the reading of the temperature was also taken, using
the formula.
% Silt + clay = (R40secs - Ra) + Rc + 100
W
% Clay = (R2hours−Rb)+Rd×100W
Where;
57
Ra = 40secs blank hydrometer reading
Rb = 2hours blank hydrometer reading
Rc = 40secs correction factor (temperature ×
0.360)
Rd = 2hours correction factor (temperature ×
0.360)
% Sand + silt + clay = 100
% Silt = (Sand + clay) – clay
Sand = 100 – (Silt + clay)
(Ibitoye, 2006 ).
58
CHAPTER FOUR
4.0 RESULTS
The results obtained from the study are presented
in Tables 4.1- 4.17.
Table 4.1 shows the light intensity (Lux/m2) of Zea
mays at week ten. It was observed that the highest
light intensity occurred in the control while the
lowest light intensity occurred in triple net (TN).
Table 4.2 shows the number of leaves of Z. mays at
week ten. It was observed that plants in loamy soil
(triple-net + ash) had the highest leaf number, whereas
the lowest value was recorded in plants grown in clay
soil (triple-net + ash).
59
Table 4.3 shows the germination (%) of maize (Zea
mays). Germination commenced at the third day for
loamy, sandy and laterite, while for clay germination
commenced at the fourth day.
Table 4.4 shows the height (cm) of maize at week
ten. The highest mean plant value was recorded in loamy
soil (triple-net + ash) while the least mean plant
height value was observed in plants grown in clay soil
(triple-net + ash).
Table 4.5 shows the leaf area (cm2) of maize at
week ten. It was observed that plants in no-net + ash
(loamy soil) were found to have the highest leaf area,
whereas the least value was recorded in plants grown in
clay soil (triple-net + ash).
60
Table 4.6 shows the stem girth (mm) of Z. mays at
week ten. The highest value of stem girth was observed
in loamy soil (triple-net + ash) while the least
value was observed in sandy soil (triple-net + ash).
Table 4.7 shows the physicochemical characteristic
of plant ash before planting. The data showed that the
pH of the ash was basic (10.08) and it also contained
important nutrients necessary for growth.
Table 4.8 shows the physicochemical analysis of
soil before planting. It was observed that all the
soils were acidic and also that loamy soil contained
more nutrient than any other soil.
Table 4.9 shows the fresh weight (g) of Zea mays at
week ten. The highest value was recorded in loamy soil
61
(triple-net + ash) while the least value was recorded
in clay soil (triple-net + ash).
Table 4.10 shows the dry weight (g) of Z. mays at
week ten. The highest value was recorded in loamy soil
(no-net + ash) while the least value was recorded in
sandy soil (triple-net + ash).
Table 4.11 shows the physicochemical
characteristics of soils in control after planting.
Table 4.12 shows the physicochemical
characteristics of soil exchangeable bases and acidity
in control after planting.
Table 4.13 shows physicochemical characteristics
of soils in no-net + ash after planting.
62
Table 4.14 shows the physicochemical
characteristics of soil exchangeable bases and acidity
in no-net + ash after planting.
Table 4.15 shows the physicochemical
characteristics of soils in triple-net + ash after
planting.
Table 4.16 shows the physicochemical
characteristics of soil exchangeable bases and acidity
in triple-net + ash after planting.
Table 4.17 shows the chlorophyll content of Zea
mays at week ten.
Table 4.1 Light intensity (Lux/m2) at week ten
Weeks Control No net + ash Triple net +ash
1 583.71a 517.00b 187.00c
2 520.43a 455.00b 216.00c
3 345.14a 304.14b 153.43c
63
4 288.00a 277.57b 158.71c
5 462.57a 421.29b 192.29c
6 478.00a 445.57b 173.00c
7 328.71a 306.29b 152.29c
8 284.43a 273.86b 98.29c
9 181.43a 163.14b 59.29c
10 186.57a 178.43b 66.14c
Means with different alphabets within different columnsare significantly different at P ≤ 0.05 using Duncan’smultiple test.
64
Table 4.2 Number of leaves at week ten
Soil Control No-net + ash Triple-net +ash
Loamy 4.60a 4.73a 4.74a
Sandy 4.13c 4.07d 3.28b
Laterite 4.27b 4.13c 3.20c
Clay 3.53d 4.46b 3.14d
Means with the same alphabets within the same columnare not significantly different at P ≤ 0.05 usingDuncan’s multiple test.
65
Table 4.3 Percentage germination of maize
Day Numberof seeds sown
Number of seed germinated/CONTROL
Number of seeds growth/No net + ash
Number of seeds germinated/ triplenet + ash
L S LT C L S LT C L S LT C1 3 0 0 0 0 0 0 0 0 0 0 0 02 3 0 0 0 0 0 0 0 0 0 0 0 03 3 2 2 2 0 3 2 2 0 3 2 3 04 3 3 2 3 2 3 3 3 2 3 2 3 15 3 3 3 3 2 3 3 3 3 3 2 3 26 3 3 3 3 2 3 3 3 3 3 2 3 27 3 3 3 3 2 3 3 3 3 3 2 3 2%Germ
100%
100%
100%
100%
66.7%
100%
100%
100%
100%
100%
66.7%
100%
66.7%
* L – Loamy
S – Sandy
LT – Laterite
C – Clay
66
Table 4.4 Plant height (cm) of Zea mays at week ten
Soil Control No-net + ash Triple-net +ash
Loamy 47.29a 52.89a 55.91a
Sandy 40.33c 39.43c 37.46c
Laterite 41.42b 42.99b 39.18b
Clay 31.69d 36.98d 29.33d
Mean with different letters within the same column aresignificantly different at P≤ 0.05 using Duncan’smultiple range test.
67
Table 4.5 Leaf area (cm2) of Z. mays at week ten
Soil Control No-net + ash Triple-net +ash
Loamy 76.19a 98.70a 66.69a
Sandy 54.46c 49.61c 34.07c
Laterite 59.87b 62.85b 40.25b
Clay 40.34d 41.74d 28.15d
Means with different letters within the same column aresignificantly different at P ≤ 0.05 using Duncan’smultiple range test.
68
Table 4.6 Stem girth (mm) of Zea mays at week ten
Soil Control No-net + ash Triple-net +ash
Loamy 4.95a 5.54a 5.91a
Sandy 4.37c 4.32d 3.14d
Laterite 4.42b 4.49b 4.48b
Clay 3.23d 4.36c 3.81c
Means with different letters within the same column aresignificantly different at P ≤ 0.05 using Duncan’smultiple range test.
69
Table 4.7 Physicochemical characteristic of plant ashbefore planting
Parameters Units AshPH 10.08% Org. C % 3.09Org matter % 5.33C/N ratio % 6.71Al Mmol/100g 41.30H+ Mmol/100g 27.20Ca Mmol/100g 60.80Mg Mmol/100g 26.40Na Mmol/100g 31.80
70
K Mmol/100g 29.60N % 0.46Avail P Mg/kg 1.77* Org. C - Percentage of organic carbon
*Org matter - Organic matter
*C/N ratio - Carbon/Nitrogen ratio
*Avail P - Available phosphorus
Table 4.8Physicochemical analysis of soils beforeplanting
Parameter
Units Loamy Sandy Laterite
Clay
pH 4.32 4.64 4.98 4.74
71
% Org. C % 2.81 1.94 2.11 1.86Orgmatter
% 4.84 3.34 3.64 3.21
C/Nratio
% 12.77 3.40 7.27 2.90
Al Mmol/100g
3.10 2.80 1.90 2.30
H+ Mmol/100g
4.80 3.90 3.60 2.70
Ca Mmol/100g
4.40 3.60 3.60 3.60
Mg Mmol/100g
4.0 1.20 0.00 2.40
Na Mmol/100g
4.10 3.30 3.60 2.80
K Mmol/100g
0.13 0.11 0.27 2.34
N % 0.22 0.57 0.29 0.64 Sand % 89.08 93.08 83.08 33.08 Silt % 1.52 1.12 1.52 1.52 Clay % 9.40 5.80 15.40 37.40Avail P Mg/kg 1.55 0.11 0.35 0.93
72
Table 4.9 Fresh weight (g) of Z. mays at week ten
Soil Control No-net + ash Triple-net +ash
Loamy 17.20a 19.63a 20.27a
Sandy 14.70b 4.93d 2.33c
Laterite 9.23c 8.10c 2.67b
Clay 2.23d 13.27b 1.67d
Means with different alphabets within the same columnare significantly different at P ≤ 0.05 using Duncan’smultiple range test.
73
Table 4.10 Dry weight (g) of maize at week ten
Soil Control No-net + ash Triple-net +ash
Loamy 3.44a 4.63a 3.37a
Sandy 3.21b 1.04d 0.47d
Laterite 2.46c 2.14c 0.83c
Clay 1.06d 3.83b 1.01b
Means with the same alphabets within the same columnare not significantly different at P ≥ 0.05 usingDuncan’s multiple range tests.
74
Table 4.11 Physicochemical characteristics of soilsin control after planting
Parameter
Units Loamy Sandy Laterite Clay
pH 4.93 4.61 4.46 4.28% Org. C % 3.39 1.05 2.41 1.80
75
Orgmatter
% 5.83 1.80 4.14 3.09
C/Nratio
% 10.94 13.13 34.43 3.27
Sand % 89.08 83.08 83.08 93.08 Silt % 1.52 1.52 29.52 1.12 Clay % 9.40 15.40 37.40 5.80
76
Table 4.12 Physicochemical characteristics ofexchangeable bases and exchangeable acidity of soils incontrol after planting
Parameter
Units Loamy Sandy Laterite
Clay
Al Mmol/100g
1.00 0.35 0.38 0.20
H+ Mmol/100g
1.60 1.10 0.55 0.55
Ca Mmol/100g
0.80 0.80 0.80 0.60
Mg Mmol/100g
1.40 1.60 1.40 0.20
Na Mmol/100g
0.11 0.05 0.19 0.40
K Mmol/100g
0.11 0.05 0.15 0.03
N % 0.31 0.08 0.07 0.55Avail P Mg/kg 57.35 27.45 4.27 40.50
77
Table 4.13 Physicochemical characteristics of soils inno-net + ash after planting
Parameter
Units Loamy Sandy Laterite Clay
PH 4.15 4.51 4.52 5.15% Org. C % 3.45 2.35 2.77 2.35Orgmatter
% 5.93 4.04 4.76 4.04
C/Nratio
% 16.43 10.22 18.47 18.08
Sand % 87.08 85.08 41.08 92.08 Silt % 1.52 1.52 25.52 0.12 Clay % 11.40 13.40 33.40 7.80
78
Table 4.14 Physicochemical characteristics ofexchangeable bases and exchangeable acidity of soils inno-net + ash after planting
Parameter
Units Loamy Sandy Laterite
Clay
Al Mmol/100g
1.20 0.85 0.45 0.35
H+ Mmol/100g
1.45 0.65 0.35 0.35
Ca Mmol/ 1.20 1.60 1.00 1.8079
100gMg Mmol/
100g0.80 1.40 1.00 1.20
Na Mmol/100g
0.19 0.17 0.13 0.05
K Mmol/100g
0.80 0.60 0.12 0.04
N % 0.21 0.23 0.15 0.13Avail P Mg/kg 56.70 11.47 4.05 29.47
80
Table 4.15 Physicochemical characteristics of soilsin triple netted-cage + ash after planting
Parameter
Units Loamy Sandy Laterite Clay
PH 4.20 4.49 4.61 5.12% Org. C % 3.43 2.24 2.79 2.12Orgmatter
% 5.90 4.10 4.40 4.02
C/Nratio
% 12.25 9.33 12.13 15.14
Sand % 89.78 84.31 40.39 93.21 Silt % 1.60 1.58 27.63 1.31 Clay % 8.61 14.11 31.98 5.48
81
Table 4.16 Physicochemical characteristics ofexchangeable bases and exchangeable acidity of soils intriple-net + ash after planting
Parameter
Units Loamy Sandy Laterite
Clay
Al Mmol/100g
1.30 0.82 0.50 0.40
H+ Mmol/100g
1.60 0.56 0.40 0.39
Ca Mmol/100g
1.70 1.30 1.40 1.40
Mg Mmol/100g
1.12 1.00 1.10 0.91
Na Mmol/100g
0.21 0.19 0.11 0.09
K Mmol/100g
0.12 0.08 0.90 0.07
N % 0.28 0.24 0.23 0.14Avail P Mg/kg 55.63 19.42 4.91 36.75
82
Table 4.17 Chlorophyll content of Zea mays at week ten
Soil Tissue
Weight (g)
Wavelength (nm)
Chlorophylla
Chlorophyll b
Total
663 645
Con
tro Loamy 0.10 0.7
30.53 1.69 1.52 3.21
83
lSandy 0.10 0.4
40.43 1.00 1.34 2.34
Laterite
0.10 0.30
0.37 0.74 1.19 1.93
Clay 0.10 0.38
0.40 0.86 1.27 2.13
No-n
et +
ash
Loamy 0.10 0.34
0.38 0.76 1.22 1.98
Sandy 0.10 0.28
0.34 0.63 1.11 1.74
Laterite
0.10 0.47
0.45 1.07 1.40 2.47
Clay 0.10 0.43
0.39 0.98 1.16 2.14
Trip
le-n
et +
ash Loamy 0.10 0.6
50.42 1.51 1.15 2.66
Sandy 0.10 0.36
0.31 0.83 0.94 1.77
Laterite
0.10 0.47
0.42 1.08 1.28 2.36
Clay 0.10 0.64
0.42 1.49 1.16 2.65
84
CHAPTER FIVE
5.0 DISCUSSION
The study on the evaluation of light intensity and
soil nutrients on the growth of Zea mays was
investigated. The treatments used for the experiment
include plant ash, light intensity (triple-net, no-net
and control) and soils (loamy, sandy, laterite and
clay). The parameters include; germination rate, plant
height, leaf number, leaf area, stem diameter, fresh
and dry weight and chlorophyll content.
The results
85
obtained from the study showed that plant ash had a
positive effect on the growth of Zea mays, this may be
due to the basic condition from ash application. There
was delay in germination with clay soil; this may be
due to the compatibility of the soil that reduced the
amount of light absorbed by the plant. Maize performed
best in loamy soil and laterite soil, but poorly in
sandy and clay soils.
The results in Table 4.4 shows that TN (triple-
net) loamy soil had the highest value (55.9cm ± 17.57)
for height after exposure. While TN clay soil had the
least value of 29.33cm ± 9.68. This may be attributed
to the nutrient status of the soil or as result of
plant Etiolation.
86
The results for leaf area and girth of the plant
were 98.70cm2 ± 47.79 and 5.91mm ± 2.67 for TN (loamy
soil). This may also be attributed to the nutrient
status of the soil.
The results obtained from the study showed that
the application of the ash material increased the soil
pH, reduced soil exchangeable acidity, exchangeable
aluminum and exchangeable hydrogen. This is because the
ash material contained basic cations and basic anions
that are able to pull H+ from exchange sites to form
H20 + Co2. Cations occupy the space left behind by H+ on
the exchange. This result is in agreement with Fageria
et al. (2007); Voundi, et al. (1998) and Ojeniyi et al. (1999)
who reported that working with 2, 4, 6 and 8tons per
hectare of ash increased the soil pH. The increase in
87
maize roots in no-net + ash and triple-net + ash was a
result of the ash, which provided basic cations, that
suppressed the toxicity of aluminum in the soil and
this enhanced the activities of the roots by creating a
better environment for the release of phosphorus, which
helps in the development and growth of the plant roots.
Franco and Mumms (1982) reported that increasing the
concentration of calcium in the soil reduced the
aluminum toxicity in bean root. Dierolf et al. (1997) also
reported that application of ash to maize allowed the
roots of maize to move up to 15 to 30cm of depth in an
acid soil. The increase of stem diameter (girth) in no-
net + ash and triple-net + ash could be as a result of
the potassium content of the ash which according to
Chude et al. (2004) is responsible for the development of
the stalks and its deficiency results in weak stalk and88
lodging of the plants. Therefore, the addition of plant
ash impacted positively on the growth parameters of
maize in the soils. As the exchangeable aluminum is
reduced, the plant roots performances were enhanced,
nutrient uptake increased and this in return led to
increase in the seedling of the plant.
5.2 Conclusion/Recommendation
The results of the study showed that the
application of plant ash increased soil pH and reduced
soil exchangeable acidity, which led to increase in
plant height, stem diameter, leaf area, root size and
stalk size of Zea mays. From the results, light
intensity, plant ash and soil types had significant
effect on the growth of maize. This study also showed
that the growth and the development of maize is highly
89
dependent on nutrient rich soils and optimum light
intensity. Further research is hereby recommended for
the field application of the treatments on maize.
REFERENCESAhn, P. M. (1993). Tropical soils and fertilizer. Journal
of Environmental Science. 13: 136-137.
Answer, C. (2006). Phototropin in plants. Annals of Botany.57: 12-16.
Ballare, C., Scopel, A. and Sanchez, R. (1991).Photo control and stem elongation in plants
neighbourhoods-effects of photon fluence rateunder natural conditions of radiation. Plant Cell andEnvironment. 14: 97-102.
Baraldi, R., Rossi, F., Francini, R., Malli, M. andNerozzi, F. (1994). Light environment growth andmorphogenesis in a peach tree canopy. PhysiologiaPlant Arum. 91: 399-345.
Batschaver, A., Rocholl, K., Nagatani, A., Furuya, M.and Schafer, F. (1998). Blue and UV-A lightregulated CHS expression in Arabidopsisindependent of phytochrome A and B. Plant Journal. 9:63-69.
90
Bennet, J.W. and Klich, M. (2003). Mycotoxins. ClinicalMicrobiology Reviews.16: 497-516.
Birch, C.J., Robertson, M.J., Humphreys, E. andHutchins, N. (2003). Agronomy of maize inAustralia in review and prospect. In: Birch, C.J. andWilson, S.R. (eds.) Versatile Maize-Golden Opportunities, 5thAustralian Maize Conference, City Golf Club, Toowoomba.Pp. 18-29.
Bjorn, L.O. (1994). Introduction In: Kendrick andKronenberg, G.H.M. (eds.). Photomophogenesis in Plants 2nd
Edition Kluwer Academic Publication, Netherland.Pp. 3-13.
Boyer, C.D. and Hannah, L.C. (1994).Kernel mutants ofcorn. In: Hallaver, A.R. (ed.) Specialty Corns. CRC PressIncorporation, Boca Raton, USA. Pp. 1-28.
Briggs, W. and Huala, E. (1999).Blue lightphotoreceptor in higher plants. Annual Review of Celland Developmental Biology. 33-62.
Buckler, E.S. and Holtsford, T.P. (1996). Zeasystematics: ribosomal ITS evidence. Molecular Biologyand Evolution. 13: 612-622.
Chude, V.O., Malgwi, W.B., Amapu, I.V. and Ano, O.A.(2004). Manual on soil fertility assessment.Published by Federal Fertilizer Department in Collaboration withNational Special Programme for Food Security, Abuja-Nigeria. Pp.32-38.
91
Colless, J.M. (1992).Maize growing. Brazilian Journal of PlantScience. 30: 20-30.
Darrah, L.L., McCullen, M.D. and Zubar, M.S. (2003). Breeding, genetics, and seed corn
production. In: White, P.J. and Johnson, L.A. (eds.) Corn:Chemistry and technology, 2nd Edition. AmericanAssociation of Cereal Chemists, Incorporation. St.Paul, Minesota, USA, Pp. 35-68.
Dhugga, K.S. (2007). Maize biomass yield andcomposition for biofuels. Crop Science. 47: 2211-2227.
Dierolf, T.S., Arya, L.M. and Yost, R.S. (1997).Waterand cation movement in an Indonesian, Ultisol.Agronomical Journal. 89: 572-579.
Doebley, J. (2004). The genetics of maize evolution.Annual Review of Genetics. 38: 37-59.
Efe, S. I. (1994). Variation in Microclimate Parametersin the different vegetation cover around Abraka..Unpublished B.sc. Dissertation. Department of Geography,Delta State University, Abraka, Nigeria.
Efe, S. I. (2006). Climate Characteristics in Abrakain: Akinbode, A. and Ugbomeh, B. A. (eds.) AbrakaRegion Occasional Publications, Department ofGeography and Regional Planning, Delta State UniversityAbraka, Pp.17.
Eleweanya, N. P., Uguru, M.I. Eneobong, E. E. andOkocha, P. I. (2005).Correlation and path
92
coefficient analysis of grain field relatedcharacters in maize (Zea mays L.) under umudikeconditions of South Eastern Nigeria. Agro-scienceJournal of Agriculture, Food, Environmental and Extension.14(1): 24-28.
Ellneskog-Staam, P., Henry, L.C. and Merker, A. (2007).Chromosome C-banding of the teosinte Zea nicaraguensisand comparison to other Zea species. Hereditas. 144:96-101.
Esau, K. (1977). The leaf: Variation in structure. In:Anatomy of Seed Plants, 2nd Edition. John Wiley andSons Incorporated, New York. Pp 351-374.
Esu, I. E. (1999). Fundamentals of Pedology. Stirling-Horden Publications Nigeria limited, Ibadan.
Fageria, N.K., Baliger, V.C. and Zobel, R.W. (2007).Yield nutrient uptake and soil chemical propertiesas influenced by liming and bron application in ano-tillage system. Communication in Soil Science and PlantAnalysis. 380(8): 1637-1652.
FAO (1992). Maize in human nutrition. Food andAgriculture Organization of the United Nation.
Farnham, D.E., Benson, G.O. and Pearce, R.B.(2003).Corn perspective and culture.In: White, P.J. andJohnson, L.A. (eds.) Corn: Chemistry and technology,2nd Edition.American Association of Cerial Chemicals,Incorporation. St. Paul, Minesota, USA, Pp. 1-33.
93
Farrell, T. and O’keeffe, K. (2007). Maize. CanadianJournal of Plant Science. 78: 30-39.
Gay, A. and Hurd, R. (1975).The influence of light onstomatal density in the tomato. New Physiologist.75:37-46.
Gratani, I. (1997). Canopy structure, verticalradiation profile and photosynthetic function in aquecus ues evergreen forest photosynthetica. NewPhysiologist. 105:139-149.
Hennig, Z., Poppe, C. Sweere, U., Martin, M. andSchafer, E. (2001). Negative interference ofendogenous phytochrome B with phytochrome Afunction in Arabidopsis. Plant Physiology.125: 1036-1044.
Hobbs, L. (2003). Corn sweeteners. In: White, P.J. andJohnson, L.A. (eds.) Corn: Chemistry and Technology, 2ndEdition. American Association of Cerial ChemicalsIncorporation .St. Paul, Minesota, USA. Pp. 635-669.
Hughes, M. (2006). Maize-insect pests. Plant Physiology.135: 56-60.
Ibitoye, A. A. (2006). Laboratory analysis, Universityof Ibadan press, Ibadan Nigeria. Pp. 202.
James, S. and Bell, D. (2000). Influence of lightavailability on leaf structure and growth of twoEucalyptus globules spp. globules provenanaces. Tree Physiology.20: 1007-1018.
94
James, T.K., Rahman, A. and Mellsop, J. (2000). Weedcompetition in maize crop under different timingsfor post-emergence weed control. New Zealand PlantProtection. 53: 269-272.
Khanna, P.K. and Raison, R.J. (2006). Fire andsoils. In: Encyclopedia of soil science. Rattan, B. (ed.).Published by Taylor and Francis LLC Group NewYork. Pp. 708-710.
Kiniry, J.R., Ritchie, J.T. and Musser, R.L.(1983).Dynamic nature of the photoperiod responsein maize. Journal of Agronomy.75: 700-703.
Lafitte, H.R. (2000). Abiotic stresses affecting maize.In: Pailwal, R.L., Granados, G. Lafitte, H.R. and Viollc, A.D. (eds.)Tropical Maize: Improvement and Production. Food andAgriculture Organization of the United Nations,Rome. Pp. 93-103.
Leal, G. (2007). Maize response to light intensity.Plant Physiology. 135: 56-63.
Lee, E.A. and Tollenaax, M. (2007).Physiological basisof successful breeding strategies for maize grainyield. Crop Science. 47(53): 5202-5215.
Mano, Y., Omori, F., Muraki, M. and Takamizo, T.(2005). QTL mapping of adventitious root formationunder flooding conditions in tropical maize (Zeamays L.) seedlings. Breeding Science. 55: 343-347.
McCutcheon, A. (2007). Maize, its nutritive and healthbenefits. Breeding Science. 57: 40-45.
95
Monjardino, P., Smith, A.G. and Jones, R.J. (2006).Zein transcription and endoreduplication in maizeendosperm are differently affected by heat stress.Crop Science. 46: 2581-2589.
Morris, R. (2008). Flood irrigated maize in the southwest of Western Australia. Environmental Protection. 45:10-20.
O’Gara, F. (2007). Irrigated maize production in thetop end of the Northern Territory. EnvironmentalProtection. 44: 9-15
Obi, M. E. (1990). A Laboratory Manual for soilphysics. University of Nigeria press, Nsukka. Pp.90.
OECD (2000). Consensus document on compositionalconsideration for new varieties of maize (Zeamays): Key food and feed nutrients, anti-nutrientsand secondary plant metabolites. Report No.ENV/JM/MONO (2002)25, Environment Directorate;Organisation for Economic Co-operation and Development,Paris, France.
OECD (2003). Consensus document on the biology of Zeamays sub-species mays (Maize). Report No. 27,Environment Directorate; Organization for Economic Co-operation and Development, Paris, France.
Ojeniyi, S.O., Adetora, A.O. and Odedina, S.A. (1999).Effect of wood ash on fertility nutrients contentand yield of okra. Paper presented at Horticultural Society ofNigeria Conference, Port Harcourt.
96
Okoruwa, A.E. and Kling, J.G. (1996). Nutrition andquality of maize. International Institute of TropicalAgriculture, Research Guide. 33: 31-34.
Paliwal, R.L. (2000). Maize types. In: Paliwal, R.L., Granados,G., Lafitta, H.R. and Viollc, A.D. (eds.) Tropical Maize: Improvementand Production. Food and Agriculture Organisation ofthe United Nations, Rome. Pp. 39-43.
Pandey, S., Ceballos, H. Magnavaca, R., Bahiafilho,A.C., Dungue-Vargas, J. and Vinasco, L.E. (1994).Genetics of tolerance to soil acidity in tropicalmaize. Crop Science. 34: 1511-1514.
Piperno, D.R. and Flannery, K.V. (2001). The earliestarchaeological maize (Zea mays L.) from highlandMexico: New accelerator mass spectrometry datesand their implications. Proceedings of the NationalAcademy of Sciences. 98: 2101-2103.
Powell, J.M.R., Pearson, A. and Hiernaux, P.H.(2004).Review and interpretation. Crop-livestockinteractions in the West Africa dry lands.Agronomical Journal. 96: 469-483.
Purseglov, J.W. (1972). Tropical crops: Monocotyledons.Crop Science. 5: 15-21.
Smith, H. (2000). Photochromes and light signalperception by plants an emerging synthesis. Nature.497: 585-591.
Srinivasan, G., Zaidi, P.H., Singh, N.N. and Sanchez,C. (2004).Increasing productivity through genetic
97
improvement for tolerance to drought and excessmoisture stress in maize (Zea mays L.). Nature. 40:227-239.
Statistical software (SAS) (2005). Horgen and enhancedSAS institution incorporation, USA.
Storrie, A., Ferguson, N, and Cook, T. (2005). Weedcontrol in summer crops. Nature. 41: 112-117.
Subbaiah, C.C. and Sachs, M.M. (2003).Molecular andcellular adaptations of maize to floodingstress. .Annals of Botany. 91: 119-127.
Udo, E. J. and Oginwale, J. A. (1996). LaboratoryManual for Analysis of soil, plant and watersamples. University of Ibadan Press, Ibadan. p.200.
USDA (2005). Germplasm Resources Information Network –(GRIN).United States Department of Agriculture,Agricultural Research Service, Beltsville.
Voundi, N.J.C.V., Demeyer, A. and Verloo M.G. (1998).Chemical effects of wood ash on plant growth intropical soils. Bioresource Technology. 63:251-260.
White, P.J. (1994). Properties of corn starch. In:Hallaver, A.R. (ed.) Specialty Corns.CRC Press Incorporation,Boca Raton, USA. Pp. 29-54.
Zhang, Z. and Qu, W. (2003). Experiment in plantphysiology. Higher Education Press, Beijing,China. p.340.
98