By Alhassan, ALH; Kyei-Baffour, N; Agyare, WA; Amponsah, W (2023).
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Greener Journal of
Science, Engineering and Technological Research ISSN: 2276-7835 Vol. 12(1), pp. 34-48, 2023 Copyright ©2023, the copyright of this article is
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Evaluation of the Performance of Sprinkler Irrigation
System for Ayoyo Cultivation using Wastewater at Zagyuri in Sagnerigu Municipal
in the Northern Region of Ghana.
Abdul Latif Husein Alhassan1,
Nicholas Kyei-Baffour2
Wilson Agyei Agyare2 and William
Amponsah2
1.
Department
of Water and Environmental Engineering, Faculty of Engineering, Tamale
Technical University, Tamale, Ghana.
2.
Department
of Agricultural and Biosystems Engineering. College of Engineering, Kwame
Nkrumah University of Science and Technology, Kumasi, Ghana.
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ARTICLE INFO |
ABSTRACT |
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Article No.: 10273122 Type: Research Full Text:
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In this study,
field tests were performed for sprinkler irrigation system. The results indicate that the average
Christiansen’s coefficient of uniformity (CU) for the sprinkler for
up-stream of the plot was the highest (95.3%) followed by the sprinkler
mid-stream (95.1%) and the least was the sprinkler down-stream (75.8%) of
the plot. The sprinkler distribution uniformity for the up-stream of the plot
was highest (99%) whiles the mid-stream was next with (92.7%) and
down-stream was the least with (67.6%). The sprinkler had average discharge
is 1.5 m3/ h. The crop water
productivity of Ayoyo (Corchorus olitorius) grown under sprinkler irrigation
was determined for the up-stream and the mid-stream with both locations
having the same value of 0.50 kg/m3 whilst the least was obtained for the
down-stream with a value of 0.44 kg/m3. It was recommended that; further
elaborate studies be conducted on the subject by considering the effects of
different pressures on the performance of sprinkler irrigation system. |
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Accepted: 31/10/2023 Published: 07/11/2023 |
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*Corresponding Author Alhassan,
Abdul Latif Husein E-mail: joelatey13@gmail.com |
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Keywords: |
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1.0 INTRODUCTION
Agriculture
is a significant consumer of global water resources, accounting for
approximately 70-80% of usage (Crovella et al., 2022). However, with
water availability diminishing, it has become imperative to enhance water
management practices within the agricultural sector. Escalating competition for
water resources among agricultural, industrial, and domestic sectors underscores
the need for ongoing advancements in water-efficient techniques for crop
production. The imperative of efficient water utilization is growing, and
alternative irrigation methods such as drip and sprinkler systems hold the
potential to substantially optimize the use of scarce water resources in crop
cultivation.
Hernandez et al., 2020). Crops like
Okra (Abelmoschus esculentus) and Ayoyo (Corchorus olitorius)
are particularly sensitive to water stress, especially during flowering and
pollination stages. Given their highwater requirements and vulnerability to
water stress, especially in light-textured soils, implementing limited or
deficit irrigation without incurring yield losses is challenging. Thus,
ensuring a consistent and uniform water supply is paramount to enhancing Ayoyo
yields. Novel approaches to augment water availability and efficiency are
imperative. Embracing irrigation technologies like drip and sprinkler systems,
designed to deliver water at a consistent rate, can serve as effective tools for
rationalizing and optimizing limited water resources (Smith et al.,
2020).
Rainfall is the single most important factor
affecting crop production (Rukuni & Carl 2004). The smallholder farming
sector in various regions faces a decline in Ayoyo (Corchorus olitorius) yields, primarily attributed to erratic
rainfall patterns, the non-uniform water requirements during different growth
stages, the sensitivity of these crops to water stress, and the competition for
water resources across various sectors due to climate change (Coelho & Or,
1999; Assouline, 2002; Wang et al., 2006).
Sprinkler
Irrigation
Sprinkler
irrigation is a modern method of irrigation where water is distributed over the
field in the form of small droplets, resembling rain, through sprinkler heads
or nozzles (Li et al., 2012). This
method allows for precise and uniform application of water, reducing water loss
due to evaporation and runoff, and increasing water use efficiency (FAO, 2012).
Sprinkler
irrigation systems can be classified into different types based on the type of
sprinkler head used, such as impact sprinklers, rotary sprinklers, and spray
sprinklers (Li et al., 2012). Impact
sprinklers are widely used in agricultural fields and operate by using the
force of water to drive a rotating arm that distributes water in a circular
pattern. Rotary sprinklers operate by rotating a series of arms with nozzles
that spray water in a specific pattern, such as full circle or part circle.
Spray sprinklers, on the other hand, operate by spraying water in a fine mist
or spray pattern, and are commonly used in smaller areas or for landscape
irrigation.
Sprinkler irrigation is suitable for a wide
range of crops, including field crops, vegetables, orchards, and lawns (FAO,
2012). It is particularly useful in areas with irregular or sloping terrain,
where other methods of irrigation may be challenging to implement (Li et al., 2012). Sprinkler irrigation can
also be used to apply fertilizers and pesticides, which can be dissolved in the
irrigation water and distributed evenly across the field, reducing the need for
separate applications (FAO, 2012). Several studies have highlighted the
benefits of sprinkler irrigation in improving water use efficiency and crop
productivity. For example, research conducted in Northern Ghana showed that
sprinkler irrigation improved crop yields and water use efficiency for crops
such as maize and tomatoes compared to traditional flood irrigation methods
(Abdul-Rahaman et al., 2015). Another
study in India demonstrated that sprinkler irrigation reduced water
consumption and improved crop yields for crops such as wheat, cotton, and
groundnut, compared to flood irrigation (Ghosh et al., 2013). However,
sprinkler irrigation also has some limitations. It requires higher initial investment
compared to other irrigation methods, such as surface irrigation, due to the
cost of equipment and installation (FAO, 2012). It also requires regular
maintenance to ensure proper functioning of sprinkler heads and nozzles, and
can be affected by wind drift and evaporation losses (Li et al., 2012).
Proper design, installation, and management of sprinkler irrigation systems,
including the use of modern technologies such as pressure regulators, weather
sensors, and automated control, can help overcome these limitations and
optimize water use efficiency and crop productivity (Abdul-Rahaman et al.,
2015; Ghosh
et al., 2013). In recent years, there
has been increasing interest in the use of sprinkler irrigation as a viable
option for farmers in peri-urban areas of Northern Ghana, where water resources
may be limited and competition for water may be high (Abdul-Rahaman et al., 2015). The use of wastewater as
a potential water source for sprinkler irrigation systems is also being
explored as a sustainable option for agricultural irrigation in water-scarce
regions (FAO, 2012). Further research and innovation in sprinkler irrigation
are expected to contribute to the adoption of more efficient and sustainable
irrigation practices for farmers in Northern Ghana and other similar regions. Figure
1 below depicts sprinkler irrigation.

FIGURE 1 Sprinkler
Irrigation (Bustan, 2008)
Sprinkler Irrigation
Factors Affecting Uniformity
Uniformity
of water distribution is a critical factor in the performance of sprinkler
irrigation systems. Several factors can affect the uniformity of water
distribution in a sprinkler irrigation system. These factors need to be
carefully considered and managed to ensure optimal performance of the system.
Some of the main factors affecting uniformity in sprinkler irrigation are:
1.
Sprinkler Nozzle Selection: The selection of the appropriate nozzle for a
sprinkler system is crucial in achieving uniform water distribution. Nozzle
size, shape, and type can significantly affect the distribution pattern and
precipitation rate of the sprinkler. It is important to select nozzles that are
matched to the specific application, including the desired radius of throw,
spacing between sprinklers, and the type of crops being irrigated (Hunt et al., 2015). Proper nozzle selection
can help achieve uniform water distribution and prevent over-watering or
under-watering of plants.
2.
Operating Pressure: The operating pressure of a sprinkler system can greatly
impact the uniformity of water distribution. Too high or too low pressure can
result in uneven distribution patterns, with some areas receiving too much
water and others not enough. Properly managing the operating pressure within
the recommended range for the specific sprinkler type and nozzle size is
essential to ensure uniform water distribution (Pereira et al., 2013).
3.
Wind Speed: Wind can have a significant impact on the uniformity of water
distribution in sprinkler irrigation systems. Wind can cause water droplets to
drift or be carried away from the intended target area, resulting in uneven
water distribution. Wind can also cause changes in the distribution pattern and
precipitation rate of the sprinkler, affecting uniformity. It is important to
consider wind speed and direction when designing and operating a sprinkler
irrigation system to minimize the impact of wind on uniformity (Li et al., 2016).
4.
Sprinkler Spacing and Overlap: The spacing between sprinklers and the overlap
of their spray patterns can affect the uniformity of water distribution. If the
sprinklers are spaced too far apart or do not overlap adequately, there may be
gaps or overlapping areas with excess water or no water. Proper spacing and
overlap of sprinklers should be considered in the design and layout of the
system to achieve uniform water distribution across the entire irrigated area
(Burt et al., 2015).
5.
Sprinkler Height and Angle: The height and angle of the sprinkler can also
affect the uniformity of water distribution. Sprinklers that are too high or
too low can result in uneven water distribution, with over-watering or
under-watering of certain areas. The angle of the sprinkler can also impact the
direction and pattern of water distribution. Proper adjustment of the sprinkler
height and angle can help achieve uniform water distribution across the entire
irrigated area (Jensen et al., 2010).
Several
factors can affect the uniformity of water distribution in a sprinkler
irrigation system, including nozzle selection, operating pressure, wind speed,
sprinkler spacing and overlap, and sprinkler height and angle. Proper
management and consideration of these factors are essential to ensure optimal
performance and uniformity in sprinkler irrigation systems
Water use efficiency
Water
use efficiency (WUE) is a critical performance indicator in irrigation systems,
including sprinkler irrigation. It is a measure of how effectively water is
utilized for plant growth and crop production. WUE is typically calculated by
dividing the amount of water used by the crop (in units of water volume, such
as cubic meters or liters) by the amount of crop yield (in units of crop
production, such as kilograms or tons).
The formula for calculating water use
efficiency (WUE) is as follows:
WUE = Crop yield / Water applied………………. (1.0)
Where:
Crop yield: the total amount of crop produced (in units of crop production,
such as kilograms or tons)
Water applied: the total amount of
water applied to the crop (in units of water volume, such as cubic meters or
liters)
Water
use efficiency is an important parameter in evaluating the performance of
sprinkler irrigation systems, as it provides an indication of how effectively
water is used in crop production. A higher WUE indicates that less water is
required to produce a certain amount of crop yield, which is desirable for
sustainable and efficient irrigation practices.
It
is important to note that WUE can be influenced by various factors, including
crop type, weather conditions, soil characteristics, irrigation management
practices, and system design. Properly managing and optimizing these factors
can help improve the water use efficiency of a sprinkler irrigation system and
maximize crop production while minimizing water consumption. Jensen, M. E.,
Haise, H. R., & Bernardi, A. (2010). Evapotranspiration and irrigation
water requirements. ASCE Press. Recent studies have shown that the measure of
water use efficiency (WUE) in irrigation systems should be based on the
transpiration efficiency (TE) of crops rather than just the ratio of yield to
total water use (Ye/ET). The TE approach considers the biomass production in
relation to the water that is actually used by the plant, and is affected by
factors such as the photosynthetic mechanism of the crop and the vapor pressure
deficit (Van Keulen, 2011; Lof, 2012). The TE approach has been found to
provide a more accurate indication of the efficiency of water use in crop
production.
Soil surface modifications, such as tillage
and the retention of surface residue, can also affect WUE by reducing soil
evaporation (E) and increasing crop transpiration (T) (Hatfield et al., 2011). Recent studies have
explored the potential advantages of using subsurface drip irrigation (SDI)
systems, which have been found to reduce soil evaporation (Solomon, 2010).
Therefore, in assessing the efficiency of
sprinkler irrigation systems, it is important to consider the transpiration
efficiency of crops and the impact of soil surface modifications on reducing
soil evaporation and increasing crop transpiration. These factors can significantly
affect the overall water use efficiency of the irrigation system, and can
inform decisions on the appropriate irrigation system design and management
practices for sustainable and efficient crop production.
2.0 MATERIALS AND
METHODS
2.1
Study Area Map
The Sagnarigu
Municipality has 79 communities, comprising of 20 urban, 6 peri-urban, and 53
rural areas. The district covers a total land size of 200.4km2 and
shares boundaries with the Savelugu-Nanton Municipality to the north, Tamale
Metropolis to the south and east, Talon District to the west and Kumbungu
District to the north-west. Geographically, the district lies between latitudes
90 16’ and 9o34’ North and longitudes 00 36’
and 00 57’
2.2 Layout of Sprinkler Plot
The sprinkler system plot or field were also divided into three (3), that
is: the up-stream, mid-stream and down-stream. Data were collected for all the
three (3) streams and analysed using the various equations of uniformity test.
This data was used to evaluate the performance of the sprinkler system. They were thirty-six (36)
catch-can arranged in each stream. Field data were collected two times in a
day, that is; morning (from 7am-7:30am) and evening (from 4pm-4:30pm). The peak crop water requirement of Ayoyo (Corchorus olitorius) is
7.5mm/day with a discharge of 1.5 m3/h
2.2.1 Discharge
Measurement
The volumetric discharge was measured with
the aid of a flexible water hose and a 17-litre bucket. The time taken to fill
the bucket was recorded and used to determine discharge using Equation 2:
..........................................................[2.0]
Where
v is the volume of water collected in
litres(l)
t is the container filter time(s) and
q is the spring flow discharge in l/s
2.2.2
Crop Water Productivity
The
assessment of crop water productivity (WP) involves a fundamental metric,
typically defined as the marketable yield divided by the total crop
evapotranspiration (Etc). However, it's worth noting that from an economic
perspective, as well as from the viewpoint of farmers, the focus often centers
on maximizing yield while optimizing the use of irrigation water resources
(Nagaz et al., 2013). This pragmatic perspective leads to the
calculation of WP as the yield in kilograms per hectare divided by the total
volume of irrigation water in cubic meters per hectare, encompassing the period
from transplanting to harvest. In the case of Okra cultivation, which employed
drip irrigation, the fresh pod yield from each stream was meticulously
determined once the green pods reached maturity. This involved a systematic
harvesting routine, with pods collected every two days throughout the harvest
period. To quantify the yield accurately, an electronic scale was employed to
weigh the harvested pods for each respective stream. Conversely, for the
'Ayoyo' crop cultivated using sprinkler irrigation, the focus was on assessing
the fresh leaf yields when the leaves reached maturity. Similar to the Okra,
electronic scales played a crucial role in precisely weighing the harvested
leaves for each respective stream. This is illustrated in the Equation 3:
![]()
Where; WP=crop
water productivity in (kg/m3)
Y= yield in (kg/ha) and TIW= total irrigation water in (m3/ha)
2.2.3 Analyses of Data
Data
recorded for both the drip and sprinkler irrigation were used to determine the
distribution patterns, discharge efficiencies and uniformity parameters
presented in the succeeding sections.
2.2.4 Discharge
Efficiency
Discharge
efficiency, Ed,
is the relationship between the water collected by the catch-cans and water
discharged by the sprinkler and the drip systems. The difference between the
actual discharge and the water collected is attributed to evaporation and drift
losses during the irrigation event, mainly as a result of environmental
conditions (Montero et al., 2002):
![]()
2.2.5 Mean Application Rate (MAR)
The
mean application rate (mm/h),
Where
q in mm3/h;
sm and
slin
m
2.2.6 Christiansen
Coefficient of Uniformity (CU)
…………………… [6]
Where,
is the mean water depth collected in all
catch-cans, n is the number of cans and xiis the water depth collected by
a catch-can, I (Christiansen, 1942 as in Keller and Bliesner, 1990).
2.2.7 Pattern
Efficiency/Distribution Uniformity
The
pattern efficiency (PE), is the ratio of the mean of 25% of the samples nearest
to the lowest, M25, to the mean of all the measured
samples. This parameter is also known as the distribution uniformity (DU):
2.2.8 Performance
criteria for system flow
Three
widely-used parameters for measuring emitter discharge uniformity are: Flow
variation, (Qvar), Uniformity coefficient (UC) and coefficient of
variation (CV).
2.2.9 Flow variation
Emitter
flow variation qvar was calculated using the equation:
Flow
variation,
……………………… [8]
Where:
Qmax = maximum emitter (drip hole) flow rate
Qmin
= minimum emitter (drip hole) flow rate
2.2.10 Uniformity
coefficient
Uniformity
coefficient, UC, as defined by Christiansen (1942) and modified to
reflect a percentage, was calculated using the equation:
Uniformity
coefficient,
………. [9]
Where:
q = discharge in (m3/s)
Mean
of discharge (q) in (m3/s)
n
= number of (drip holes) emitters evaluated.
2.2.11 Coefficient of
variation
Uniformity
coefficient,
…………………………………. [10]
Where:
s = standard deviation of (drip flow) emitter flow rate
Mean of discharge (m3/s)
2.2.12 Catch-can Description
and Set-up for Sprinkler Irrigation
For the purpose of
conducting the irrigation test, standardized cans with identical dimensions,
measuring 84mm in diameter and 130mm in height, were meticulously selected. It
is noteworthy that the guidance of irrigation experts regarding the recommended
number of cans per test zone, typically ranging from 16 to 20 cans, was adhered
to, as advised by Wilson and Zoldoske in 1997. Additionally, in line with the
recommendations set forth by the Irrigated Crop Management Centre in 2002,
which advocate for a minimum of 30 cans, each with a minimum height of 100mm,
to assess sprinkler irrigation uniformity, this study thoughtfully employed 36
catch-cans. This number of catch-cans ensured the evaluation of the water
distribution pattern for sprinkler irrigation while maintaining compliance with
established standards. In the context of field and laboratory tests, catch-cans
are commonly arranged in either a rectangular grid or in one or more radial
configurations. For the specific test conducted in this study, the decision was
made to employ the full rectangular grid setup. This choice was made based on
the rationale that it provides more representative and reliable data,
particularly when there are prevailing wind conditions during the test. Figure 3
depicts catch-cans used to collect water in Ayoyo farm.

FIGURE 3:
Catch-Cans Used to Collect Water in Ayoyo Farm (Field
Studies, 2023)
2.2.13 Materials
The materials used
for the research were:
• ˝ inch (0.0127m)
PVC pipe 6m in length
• ˝ inch (0.0127m)
end caps
• ˝ inch (0.0127m)
elbow
• ˝ inch (0.0127m) tap
• 2 mm drill bit
• Hydro sensor II
(used to monitor the soil moisture content of the field)
• Geotextile layer
(used in association with soil, has the ability to separate, filter, reinforce,
protect, or drain)
• Flexible copper
wire (core)
• Storage tank
(2000Litres, use to store water)
• Metal stand raise height of water flow for the storage
tank (height of the metal stand is 2.5m)
• Funnel (used to channel liquid or
fine-grained substances into containers with a small opening)
• Recordable rain
gauge (Truchek_200, commercial name) (used to measure rainfall)
• Measuring tape (used to measure distance)
• Measuring cylinder (used to measure volume
of liquids)
Stop watch (used to
measure the amount of time elapsed from a particular time when it is activated
to the time when the piece is deactivated)
• Collection cans (used to collect water)
·
Fittings
or pipe connector fittings
·
Spray
tubes
·
Flow control devices
·
Filters
·
Micro
spray tubes 40mm
·
Offtake
valves and saddles 40mm
·
P.E
end cap 32mm
·
Air
release valve 1 inch
2.2.14 Detailed Soil
Survey
Composite
soil samples were meticulously collected at a depth of 30cm from distinct
locations at the site, considering up-stream, mid-stream, and down-stream
positions for subsequent analysis of various physical and chemical soil
properties. These analyses were performed at the Savannah Agricultural Research
Institute (SARI) soil laboratory in Nyankpala. Notably, the soils in the area
displayed a limited depth, averaging less than 30 cm due to the presence of
hardpan and lateritic outcrops. Several essential soil physico-chemical
properties were examined, including pH, CEC (Cation Exchange Capacity),
potassium (K), calcium (Ca), nitrogen, and soil texture. Total nitrogen content
was determined using the Kjeldah method (Bremner and Mulvancy, 1982), while
phosphorus (P) levels were analyzed using the Bray-P solution method.
Additionally, potassium (K) concentrations were ascertained using the flame
photometer method recommended by the United States Salinity Laboratory Staff
(1954). pH and organic carbon (OC) content were determined using the Walkley
and Black technique (1934), while calcium (Ca) and magnesium (Mg) were assessed
via the Ammonium acetate method (Motsara and Roy, 2008; Ogunddare et al.,
2015; Peter, 2018). These analyses were conducted to ensure soil suitability
for drip irrigation. In addition to laboratory assessments, on-site soil water
infiltration tests were carried out, encompassing both up-stream and
down-stream locations. These tests aimed to determine the maximum infiltration
capacity or hydraulic conductivity of the soils in their natural environment. Unbiased
plotting positions were employed for the collected data. Knowledge of soil
infiltration rates was vital not only for calculating crop water requirements
but also for selecting appropriate drip emitter discharge rates to prevent
surface water runoff and water wastage at the Zagyuri site within the drip
irrigation system. The double ring infiltrometer method was utilized for the
field infiltration rate measurements, requiring specific equipment, including
the double ring infiltrometer, wooden support for driving the rings into the
soil, a mallet, bucket, measuring jug, stopwatch, notebook, measuring tape or
ruler, and an adequate water supply. The method involves two concentric metal
rings, with measurements taken within the inner cylinder to assess soil
infiltration properties. The outer cylinder serves to guide water flow downward
and prevent lateral spreading during the test.
The
procedure for the infiltration test is as follows:
·
Drive the
30cm diameter ring at least 15cm into the soil, using timber to protect the
ring from damage. Maintain a vertical ring position, with approximately 12cm
protruding above the ground.
·
Install the
60cm ring into the soil or construct an earth bund around the 30cm ring,
ensuring it reaches the same height as the ring. Place hessian inside the
infiltrometer to protect the soil surface during water pouring.
·
Initiate
the test by rapidly pouring water into the 30cm ring until it reaches a depth
of approximately 70-100mm. Simultaneously, add water to the space between the two
rings to create a water barrier that prevents lateral water spread.
·
Record the
starting time of the test and note the water level on the measuring rod or
ruler.
·
After 1-2
minutes, record the drop in water level within the inner ring on the measuring
rod and replenish the water to restore it to the original level. Maintain a
consistent water level outside the ring, similar to the inside.
·
Continue
the test until the drop in water level remains consistent over the same time
interval. Initially, take frequent readings (e.g., every 1-2 minutes) and
gradually extend the intervals between readings (e.g., every 20-30 minutes) as
the test progresses.
·
The
collected data were subsequently analyzed using the well-known Kostiakov
infiltration equation (Kostiakov, 1932). This model suggested a formula which
assumes that at time t=0, the infiltration rate is infinite and at time t the rate approaches zero. This equation is
given by:
![]()
Where;
I =
Cumulative infiltration rate
M = A
measure of initial rate of infiltration and structural condition of the soil
t = time
n = Index
of soil structural stability
Taking the
logs of both sides gives:
![]()

Figure 4 Infiltration Test Conducted at
Zagyuri Site (field studies, 2023)
3.
RESULTS AND DISCUSSION
3.1
Soil Survey and Infiltration
The average infiltration rate for the site is
160.25 mm/h. The results of the infiltration test suggest that the soils of the
site belong to hydrologic soil group A/B.
Group A is sand, loamy sand or sandy loam types of soils while Group B
is silt loam or loam (Nielsen et al.,
2017) it has a moderate infiltration rate when thoroughly wetted. It has low
runoff potential and high infiltration rates even when thoroughly wetted. These
soils have high to moderate rate of water transmission. This also, means
that a 160.25 mm/h layer of water on the soil surface will infiltrate in one
hour. This rate also falls above 13 - 76 mm/h which was started by Waller and
Yitayew (2016) to be the range of sandy loam soils. The infiltration rate of
160.25 mm/h indicates a relatively high rate of water absorption by the soil.
This could be beneficial for irrigation practices, as it suggests that the soil
can quickly accept and distribute water to plant roots. High infiltration rates
can reduce the risk of runoff and water wastage, leading to improved irrigation
efficiency. This is consistent with the findings of (Badr et al.,2022) who concluded that the soil with a high infiltration
rate can support efficient irrigation methods like surface or subsurface drip
irrigation, enabling better control over water application and reducing water
losses due to runoff. As such the soils are suitable for sprinkler
irrigation. The detailed results are showed in figure 5, figure 6 and Table 1.
Table 1. Soil Physico-Chemical Properties
Results
|
Treatment |
pH (1:2.5 H2O) |
%O.C |
% Total N |
P (mg/kg) |
K (mg/kg) |
Ca (mg/kg) |
Mg (mg/kg) |
CEC (cmol/kg) |
% Sand |
% Silt |
% Clay |
Texture |
|
Upstream |
5.30 |
0.38 |
0.04 |
64.47 |
110.40 |
133.60 |
126.50 |
10.89 |
54.00 |
25.60 |
20.40 |
Sandy Loam |
|
Downstream |
5.40 |
0.47 |
0.04 |
69.36 |
114.29 |
162.56 |
137.89 |
12.65 |
43.43 |
29.71 |
27.29 |
Loam |
(Field studies, 2023)

Figure 5 Downstream Infiltration Curve (F=70.5mm/H) (Field Studies,
2023)

Figure 6 Upstream Infiltration Curve (F = 250 Mm/H)
(Field Studies, 2023)
3.2.1 pH
The pH
values for both up-stream and down-stream treatments are slightly acidic, with
up-stream having a pH of 5.3 and down-stream having a pH of 5.4. These values
indicate a soil pH that is within an acceptable range for most crops. However,
specific crop requirements and soil amendment recommendations should be
considered to optimize soil pH for desired plant growth.
3.2.2
Organic Carbon Content (%O.C)
The organic
carbon content is an important indicator of soil fertility and nutrient
availability. The up-stream treatment has an organic carbon content of 0.38%,
while the down-stream treatment has a slightly higher value of 0.47%. These
values suggest that the down-stream treatment may have slightly higher organic
matter content, indicating a potentially higher fertility level. Adequate
organic matter in the soil is crucial for nutrient retention, water holding
capacity, and overall soil health. Soils with organic carbon values between 0.5
and 1.5% are considered to be low in organic carbon content by Tadese (1991).
Thus, the soil of the site was found to be less than 3% indicating the soil
health to be poor (Tequam and WSP, 2017).
3.2.3 Total
Nitrogen (%N)
The total
nitrogen content is essential for plant growth and is an important component of
soil fertility. The up-stream and down-stream have the same values for total
nitrogen content of 0.04 (%N). Soil TN availability of < 0.05 % as very low, 0.05 -
0.12 % as low, 0.12 - 0.25 % as moderate and > 0.25 % as high was classified
by Tadese (2017). According to this classification, analysis of soil samples
indicated a very low level of total N indicating that the nutrient is a
limiting factor for optimum crop growth. This is in agreement with similar
studies which reported Nitrogen to be the most limiting soil nutrient because
of its high volatility and the fact that it can be easily leached (Kebede, 2019).
3.2.4 Phosphorus (P), Potassium
(K), Calcium (Ca), and Magnesium (Mg)
The
concentrations of these macronutrients in the soil play a vital role in plant
growth and development. In the Upstream treatment, phosphorus, potassium,
calcium, and magnesium are reported as 64.47 mg/kg, 110.4 mg/kg, 133.6 mg/kg,
and 126.5 mg/kg, respectively. The Downstream treatment shows slightly higher
concentrations for these nutrients, with values of 69.36 mg/kg, 114.29 mg/kg,
162.56 mg/kg, and 137.89 mg/kg, respectively. These values suggest that the
downstream treatment may have a slightly higher nutrient availability compared
to the upstream treatment, which can positively impact plant growth and
productivity.
3.2.5 Cation Exchange Capacity
(CEC)
The CEC
indicates the soil's ability to retain and exchange cations, which are
essential for nutrient availability to plants. The Upstream treatment has a CEC
of 10.89 cmol/kg, while the Downstream treatment has a higher CEC of 12.65
cmol/kg. A higher CEC implies that the soil has a greater capacity to retain
and release nutrients to plants, which is beneficial for crop production.
3.2.6 Soil Texture
The soil
texture provides information about the relative proportions of sand, silt, and
clay particles in the soil. The up-stream treatment is classified as sandy
loam, with 54% sand, 25.6% silt, and 20.4% clay. The down-stream treatment is
classified as loam, with 43.43% sand, 29.71% silt, and 27.29% clay. These soil
textures indicate different water-holding capacities and drainage characteristics,
which can influence plant growth and management practices. The result is in
harmony with Buri et al., 2012;
Shaibu et al., 2017 who reported that soil textures within the Northern
zones are dry and vary from sand through sandy loam to silt and are relatively
poor in clay content.
3.3 Design of the
Spray Tube System or Sprinkler System
The spraying tube used for this study was a 100 m
flexible tube but 80 m was used on the field. The distance between two spray
tube is 3 m. There are specified holes created across the tubes and there are 30
holes per line and 10 lines. The distance between two holes is 30 cm (0.3m).

Figure
7: Design of the Spray Tube System
3.4 Sprinkler
Uniformity Coefficient
The
coefficient of uniformity from the up-stream was evaluated as 95.3%, which was
comparatively higher than that of Keller & Bliesner (1990) observed
elsewhere (85%). Also, the coefficient of uniformity from the mid-stream was
evaluated as 95.1% which was also comparatively higher than that of Kellers
&Bliesner (1990) observed elsewhere (85%). The down- stream was also
evaluated as 75.8% which was comparatively lower than that of Keller
&Bliesner (1990) observed elsewhere (85%). The low down- stream value for
the uniformity coefficient can be attributed to the lower volume of water
received at the down-stream. Also, the results obtained from the studies agreed
with the results attained by Batchelor at
el., (2014) which had high CU at the up-stream followed by mid-stream and
the down-stream had the least CU. This
is illustrated in figure 8.
3.5 Sprinkler Distribution Uniformity
The
distribution uniformity was also evaluated from the data gathered. The
up-stream distribution uniformity was evaluated as 99%, the mid-stream was
92.7% and the down-stream was also evaluated as 67.6%.
These figures showed that, the distribution
uniformity for the up-stream and mid- stream was high; this means that the
water was distributed uniformly across the field except the down-stream which
was low as 67.6%. The low down-stream value for the sprinkler distribution
uniformity can be attributed to the lower volume of water received at the
down-stream. Also, the results obtained from the studies agreed with the
results attained by Batchelor et al.,
(2014) which had high DU at the up-stream followed by the mid-stream and the
down-stream had the least DU. This is illustrated in figure 9
3.6 Mean Application Rate of Sprinkler
Irrigation
The mean application rate from the sprinkler
irrigation system was 3.75 mm\h. The average soil infiltration rates observed
was 160.25 mm/h. Thus, this particular sprinkler could perform without runoff.
The results obtained from the studies agreed with the results attained by
Valenzuela et al., (2017) which had
mean application rate of 3.74 mm/h.
3.7
Crop Water Productivity of Ayoyo
There was difference in Ayoyo (Corchorus
olitorius) fresh leaves yield under sprinkler irrigation. The up-stream
recorded the higher yield of 900 kg/ha followed by the mid-stream of 880 kg/ha
and the down-stream of 544 kg/ha. The differences in yield are attributed to
the amount of water received by each of the stream. The results obtained from
the studies agreed with the results attained by Valenzuela et al., (2017) which was in a range of 760 kg/ha-900 kg/ha. The
results obtained from the studies also agreed with the values attained from FAO
(2020) which was in a range of 700 kg/ha-930 kg/ha. However, the results
obtained from the studies were lower than the results recorded by Nagaz et al., (2013) in Tunisia which were in
the ranged of 1000 kg/ha-1200 kg/ha. This could be due to differences in geographical
locations. The up-stream and the mid-stream recorded the same values of crop
water productivity of 0.50 kg/m3 and the down-stream recorded the
least crop water productivity value of 0.44 kg/m3. The crop water
productivity results also agreed with the results attained by Valenzuela et al., (2017) which was in a range of
0.43 kg/m3-0.50 kg/m3. The crop water productivity results agreed with
the values attained from FAO (2020) which were in the ranged 0.39 kg/m3-0.67
kg/m3. This is illustrated in Table 2
Table 2 Crop Water Productivity of Ayoyo
|
DIVISION |
TOTAL WATER (m3/ha) |
YIELD (kg/ha) |
Productivity (kg/m3) |
|
UP-STREAM |
1787.4 |
900 |
0.50 |
|
MID-STREAM |
1687.1 |
850 |
0.50 |
|
DOWN –STREAM |
1213.3 |
542 |
0.44 |
(Field studies, 2023)
4.0 CONCLUSION
The average infiltration rate for the site is 160.25 mm/h. The
results of the infiltration test suggest that the soils of the site belong to
hydrologic soil group A/B. Group A is
sand, loamy sand or sandy loam types of soils while Group B is silt loam or
loam. It has a moderate infiltration rate when thoroughly wetted. It has low
runoff potential and high infiltration rates even when thoroughly wetted. These
soils have high to moderate rate of water transmission. This also, means
that a 160.25 mm/h layer of water on the soil surface will infiltrate in one
hour.
From the determined
sprinkler mean application rates (MAR) (4.63mm/h) and the basic soil
infiltration rate (160.25mm/h), the impact sprinkler tested in this study was
suitable and could therefore be used satisfactorily without runoff. Both the
up-stream and the mid-stream could also be employed satisfactorily without any
runoff.
Also, there was
difference in Ayoyo (Corchorus olitorius) fresh leaf’s yield
under sprinkler irrigation. The up-stream recorded the higher yield of 900kg/ha
followed by the mid-stream of 880kg/ha and the down-stream of 544kg/ha. The
differences in yield are attributed to the amount of water received by each of
the stream. For the crop water productivity of Ayoyo under sprinkler
irrigation system, the up-stream and the mid-stream recorded the same value of
0.50kg/m3 and the down-stream recorded the least value of 0.44kg/m3.
For the sprinkler irrigation system, the
up-stream data produced higher/better results than the mid-stream and the
down-stream for all the parameters studied i.e. mean application rate (MAR),
coefficient of uniformity (CU) and pattern uniformity or distribution
uniformity (PE/DU). Also, the up-stream data from the sprinkler gave very good
results as regards, the coefficient of uniformity (CU) and pattern uniformity
or distribution uniformity (PE/DU) which were above standard values stated in literature.
For the soil texture analysis, he up-stream treatment is classified as sandy loam, with 54%
sand, 25.6% silt, and 20.4% clay. The down-stream treatment is classified as
loam, with 43.43% sand, 29.71% silt, and 27.29% clay. These soil textures
indicate different water-holding capacities and drainage characteristics, which
can influence plant growth and management practices. The total nitrogen content
is essential for plant growth and is an important component of soil fertility.
The up-stream and down-stream have the same values for total nitrogen content
of 0.04 (%N). Soil
TN availability of < 0.05 % as very low, 0.05 - 0.12 % as low, 0.12 - 0.25 %
as moderate and > 0.25 % as high. The organic carbon content is an important indicator of soil
fertility and nutrient availability. The up-stream treatment has an organic
carbon content of 0.38%, while the down-stream treatment has a slightly higher
value of 0.47%. These values suggest that the down-stream treatment may have
slightly higher organic matter content, indicating a potentially higher
fertility level. Adequate organic matter in the soil is crucial for nutrient
retention, water holding capacity, and overall soil health. The pH values for
both up-stream and down-stream treatments are slightly acidic, with up-stream
having a pH of 5.3 and down-stream having a pH of 5.4. These values indicate a
soil pH that is within an acceptable range for most crops.
Acknowledgement
I am
grateful to all those who in diverse ways contributed to the successful
completion of this research work. I thank the Almighty God, to whom all
knowledge, wisdom and power belong for sustaining me in good health, sound
judgement and strength to move on. Special appreciations go to my brother Mr.
Ishmael Alhassan who helps in analyzing of the data. I also thank Ghana
government for timely disbursing the book and research allowance which is used
for publication of research works.
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|
Cite this Article: Alhassan,
ALH; Kyei-Baffour, N; Agyare,
WA; Amponsah, W (2023). Evaluation of the
Performance of Sprinkler Irrigation System for Ayoyo
Cultivation using Wastewater at Zagyuri in Sagnerigu Municipal in the Northern Region of Ghana. Greener Journal of Science, Engineering
and Technological Research, 12(1): 34-48. |