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M Imam Mohammed et al Int. Journal of Engineering Research and Applications www.ijera.com
ISSN : 2248-9622, Vol. 4, Issue 3( Version 1), March 2014, pp.314-318
www.ijera.com 314 | P a g e
Effect of Electrical Conductivity on the Soil of Irrigated
Farmlands of Kaduna Metropolis Nigeria
W.L.O Jimoh1
and Mahmud Imam Mohammed2
1
Department of Pure and Industrial Chemistry, Bayero University, Kano Nigeria.
2
Department of Applied Science, College of Science and Technology, Kaduna Polytechnic
ABSTRACT
The objective of this research work is to assess the level of electrical conductivity in the soil of irrigated
farmlands of Kaduna metropolis using conductivity meter. It was found that lowest electrical conductivity of
1.14 µScm-1
was obtained from Badiko samples and the highest from Kawo with conductivity of 2.63 µScm-1
.
It was also found that from the ANOVA p = 0.000<0.05 shows that there is significant differences in the
electrical conductivity of soil across the various sampling sites. The real differences of soil conductivity was
further analyzed by a post-hoc test using the Duncan Multiple range test with samples from Badiko and
Nasarawa having the least soil conductivity. In the second homogeneous subgroup there is Danmani, Abakpa,
Makera, Doka etc. The third subgroup include Rigasa, Kabala, Barnawa,Kakuri, Kawo, Malali while the
highest soil conductivity fall in the fourth subgroup which include Kawo and Rigachikun (control sites). Infact
most of the samples were moderately saline while some are non saline, as a result of human activities occurring
in such sites, hence, increase the mobility of heavy metals in the soil. Thereby leading to the toxicity and
polluting the soil as well as reducing its ability in the production of crops and vegetables in the affected
agricultural areas.
Keywords: Soil, conductivity Meter, Kaduna Metropolis, Nigeria.
I. INTRODUCTION
Electrical conductivity (EC) is the ability of
a material to transmit (conduct) an electrical current
and is commonly expressed in units of milliSiemens
per meter (mS/m).
Soil electrical (EC) is a measurement that
correlates with soil properties that affect crop
productivity, including soil texture, cation exchange
capacity (CEC), drainage conditions, organic matter
level, salanity and subsoil characteristic
The electrical conductivity of soil varies
depending on the amount of moisture held by soil
particles. Sands have a low conductivity, silts have a
medium conductivity and clays have a high
conductivity. Soil electrical conductivity (EC) can be
related to specific soil properties that affect crop
yield such as topsoil depth, PH, salt concentrations
and available water – holding capacity.
Soil is a dynamic layer in which many
chemicals, physical and biological activities are
going on constantly. It is not a lifeless zone but an
active system having inputs and outputs of energy
and matter. The soil has become adjusted to a
prevailing condition of climate and plant cover may
change when the prevailing condition change
(Ademoroti, 1996).
Irrigation is the artificial means of water
supply to the agricultural crops ranging from surface
irrigation, micro sprayer and low-head barber
irrigation. Irrigation is design to permit farming in
arid regions and offset drought in semi-arid or semi
humid regions.
The type of irrigation system employed in
the farmlands of the Kaduna metropolis is the surface
irrigation where water is applied directly to the soil
surface through channel which varies in size from
individual furrow to large basin.
Domestic waste water contains metal from
metabolic waste, corrosion of water pipes and
consumer products. Industrial effluents and water
slug may substantially contribute to the metal loading
(Zapella, 2003).
In Nigeria the use of polluted water in the
immediate surroundings of big cities for growing of
vegetables is a common practice. Although this water
is considered to be rich source of organic matter and
plant nutrients, it also contains sufficient amounts of
soluble salts and heavy metals like Fe, Mn, Cu, Zn,
Pb, etc. When such water is used for cultivation of
crops for a long period, heavy metals may
accumulate in soil and may be toxic to the plants.
(Kirkhan, 1983).
Long term waste water irrigation may lead
to the accumulation of heavy metals in agricultural
soils and plants. Food safety issues and potential
health risks make this as one of the most serious
environment concerns (Cui et al., 2004).
Consequently, with the increasing use of fertilizers,
RESEARCH ARTICLE OPEN ACCESS
M Imam Mohammed et al Int. Journal of Engineering Research and Applications www.ijera.com
ISSN : 2248-9622, Vol. 4, Issue 3( Version 1), March 2014, pp.314-318
www.ijera.com 315 | P a g e
biosolid and other related amendments to boost
agricultural production and increasing reuse of
treated and untreated wastewater as irrigation water,
especially in the developing regions of the world,
there is need to adequately assess the possible
environmental impacts of such applications and
agricultural practices.(Tijani and Agakwu)
The aim of this research work is to assess
the effect of electrical conductivity on the soils used
as agricultural areas of Kaduna metropolis so as to
ascertain the extent of its pollution.
II. MATERIAL AND METHOD
Sample and Sampling:
Soil samples were randomly collected in a
hole of 10cm deep which was dug from the irrigated
farmlands where vegetables were grown and irrigated
with water. These samples were then stored in
polythene bags and taken to the laboratory and dried
in an oven at a temperature of 1050
C.
The dried soil samples were ground with
mortar and pestle and sieved with 2mm sieve.
III. DESCRIPTION OF THE
SAMPLING SITES
Soil samples for heavy metal determination
were collected from twenty one (21) irrigation sites
of the Kaduna metropolis. These sites were Kabala
(KBL), Danmani (DMN), Rigasa (RGS), Barnawa
(BNW), Makera (MKR), Kakuri (KKR), Badiko
(BDK) Nasarawa (NAS, Malali (MAL), Kudenda
(KUD), Kinkinau (KKN), Kawo (KWO), Unguwan
Rimi (URM), Unguwan Sanusi (UNS), Tudun Wada
(TDW), Doka (DKA), Unguwan Dosa (UDS),
Kabala Costain (CTA), Kurmin Mashi (KMS) and
Abakpa (ABK). In this research work soil sample
from Rigachikun (RCK) irrigation site was taken as
control site. Figure 1.0 shows the detail map of the
sampling sites.
Fig 1.0 Map of the Sampling points and the
control site
SAMPLE PREPARATION
Determination of conductivity
20g of the ground soil sample was taken into a
beaker and 100cm3
of distilled water was added and
mixed thoroughly. The sample was allowed to stand
for 10 minutes. The sample solution was then
decanted into another clean beaker. The conductivity
meter of the sample solutions were determined using
a model ELE 470 conductivity metre. This
conductivity metre was turned on and the probe was
inserted into the decanted suspended solution of soil
samples. The conductivity of each solution was taken
and recorded. The probe was removed from the
samples and thoroughly rinsed with distilled water.
The procedure was repeated for all the samples
collected from the various farmlands in the present
study.
IV. RESULTS AND DISCUSSION
The mean conductivity of the soil from the
various irrigation sites of the Kaduna metropolis are
summarized in the below Table 1.0.
Fig 1.0: Distribution of conductivity in soil from different sites of the Kaduna metropolis.
95% Confidence Interval for
Mean
Lower
Bound
Upper
Bound
SL (KBL) 1.793 0.301 0.174 1.045 2.541
SL (DMN) 1.570 0.044 0.025 1.462 1.678
SL (RGS) 1.760 0.052 0.030 1.631 1.889
SL (BNW) 1.827 0.237 0.137 1.238 2.415
SL (MKR) 1.720 0.017 0.010 1.677 1.763
SL (KKR) 1.990 0.060 0.035 1.841 2.139
SL (BDK) 1.138 0.844 0.488 0.960 3.235
SL (NAS) 1.470 0.070 0.040 1.296 1.644
SL (MAL) 2.537 0.474 0.273 1.360 3.713
SL (KKR) 1.960 0.442 0.255 0.861 3.059
SL (KKN) 2.297 0.614 0.355 0.771 3.822
SL (KWO) 2.633 0.754 0.435 0.760 4.506
SL (URM) 2.260 0.862 0.497 0.120 4.400
M Imam Mohammed et al Int. Journal of Engineering Research and Applications www.ijera.com
ISSN : 2248-9622, Vol. 4, Issue 3( Version 1), March 2014, pp.314-318
www.ijera.com 316 | P a g e
SL (UNS) 2.343 0.560 0.323 0.952 3.735
SL (TDW) 2.453 0.912 0.527 0.187 4.719
SL (DKA) 1.723 0.059 0.034 1.578 1.869
SL (UNS) 1.610 0.036 0.021 1.520 1.700
SL (CTA) 2.110 0.235 0.136 1.526 2.694
SL (KMS) 1.723 0.211 0.122 1.200 2.247
SL (ABK) 1.620 0.062 0.036 1.465 1.775
SL RCK (Control) 2.643 0.625 0.361 1.092 4.195
Table 1.0 shows the electronic conductivity
soil samples obtained from the 21 irrigation sampling
sites of the Kaduna metropolis. Conductivity of the
Soil Samples
The electrical conductivity of the soil
samples from the irrigation sites indicated the lowest
conductivity of 1.14 µScm-1
from Badiko sample and
highest from Kawo with conductivity of 2.63 µScm-1
and were both lower than the conductivity value of
3.00µScm_1
obtained in soil from Zaria 3.00µscm-1
(
Uba et al.,2008). The higher conductivity value of the
soil obtained from Zaria when compared to that
obtained in this work may be attributed to the
presence of certain element such as
Na,Ca,Mg,K,Fe,Cu Zn etc were constituent of the
soil and were abundance in the former than in the
later.
Table2.0: ANOVA Table for Conductivity
Source of Variation Sum of Squares DF Mean Square F Sig.
Between Groups 10.295 20 0.515 2.337 0.010
Within Groups 9.250 42 0.220
Total 19.545 62
From the ANOVA table 2.0 above,
05.0010.0 p there is significant difference in
the conductivity across the various sample sites. The
real differences of conductivity further be analyzed
by a post-hoc test using the Duncan Multiple range
test in the table below; where means of homogeneous
subgroups are clearly displayed. Moreover, the mean
plots that follow clearly depict the mean values of the
conductivity across the various locations.
Table 3.0: Duncan Test for Conductivity
Subset for alpha = 0.05
1 2 3
4
Badiko 1.14
Nasarawa 1.47
Danmani 1.57
Unguwan Dosa 1.61
Abakpa 1.62
Makera 1.72
Doka 1.72
Kurmin Mashi 1.72
Rigasa 1.76
Kabala 1.79
Barnawa 1.83
Kudenda 1.96
M Imam Mohammed et al Int. Journal of Engineering Research and Applications www.ijera.com
ISSN : 2248-9622, Vol. 4, Issue 3( Version 1), March 2014, pp.314-318
www.ijera.com 317 | P a g e
Kakuri 1.99
Costain 2.11
Unguwan Rimi 2.26
Kinkinau 2.30
Unguwan Sanusi 2.34
Tudun Wada 2.45
Malali 2.54
Kawo 2.63
Rigachikun (Control) 2.64
Sig. 0.070 0.066 0.063 0.051
From the Duncan multiple range tests
displayed in Table 3.0, Badiko and Nasarawa, have
the least conductivity. In the second homogeneous
subgroup we have Danmani, Unguwan Dosa,
Abakpa, among others. Similarly, in the third
homogeneous subgroup we have Rigasa, Kabala,
Barnawa, among others. The highest conductivity fall
in the fourth subgroup; which include only Kawo and
Rigachikun. This is depicted in figure 2.0
0
0.5
1
1.5
2
2.5
3
BadikoN
asaraw
a
D
anm
ani
U
nguw
an
D
osa
Abakpa
M
akera
D
oka
Kurm
in
M
ashi
R
igasa
Kabala
Barnaw
aKudenda
Kakuri
C
ostain
U
nguw
an
R
im
iKinkinau
U
nguw
an
Sanusi
Tudun
W
ada
M
alali
Kaw
o
R
igachikun
(C
ontrol)
Sampling Site
Meanconductivity(uS/cm)
Series1
Series2
Series3
Series4
Fig.2.0: A mean Plot for Conductivity
However, all conductivity values of the
analyzed soil in this research work were within the
normal range ,that is, 0 - 200µscm-1
as reported by
Zaku et al., (2011). The soil electrical conductivity
varies significantly from one farmland to another (p <
0.005). Boulding (1994) classified electrical
conductivity of soil as non – saline < 2; moderately
saline 2 – 8; very saline 8 – 16 ; extremely saline
>16. From the result of this research work, most of
the samples were moderately saline while some are
non saline, as a result of human activities occurring
in such sites . Hence, increase the mobility heavy
metals in the soil.
V. CONCLUSION
In the present study, the electrical
conductivity of different irrigation sites of Kaduna
metropolis were determined and found that most of
these sites were within the normal range ,that is, 0 -
200µscm-1
as reported by Zaku et al., (2011). Also
M Imam Mohammed et al Int. Journal of Engineering Research and Applications www.ijera.com
ISSN : 2248-9622, Vol. 4, Issue 3( Version 1), March 2014, pp.314-318
www.ijera.com 318 | P a g e
most of the samples were moderately saline
while some are non saline, as a result of human
activities occurring in such sites. Hence, increase the
mobility of heavy metals in the soil. Thereby leading
to toxicity and polluting the soil as well as reducing
its ability in the production of crops and vegetables in
the affected agricultural areas..
VI. ACKNOWLEDGEMENT
The Authors were grateful to the
management of Kaduna Polytechnic for sponsoring
this research work.
REFERENCES
[1] Ademoroti C.M.A (1996): Soil, water and
air environmental chemistry and
texiocology. Foludex Press Ibadan, 1st
Edition Pp 30-34.
[2] Boulding, J. R (1994). Description and
sampling of contaminated soils. Alfeid
Guide. 2nd
Edn. Lewis publishers, Boca
Raton, FL. Pp 5
[3] Cui, Y.J, Zhu, Y.G, Zhain R.H, Chen, D.Y,
Huang Y.Z, Qui Y and Liang J.Z (2004).
Tranfer of metals from nrar a smelter in
Nanning., China. Environmental
International 30: 785 – 791.
[4] Kirkhan, M.B (1983), study on
accumulation of heavy metals in soil
receiving sewage and effluent water. Agric.
Ecosystem, Environment 9:251.
[5] Tijani, M.N and Agakwu, A.A (2007) An
assessment of soil – plant transfer of trace
metals and contamination of shallow
groundwater under amendment irrigated
fields. African crop science conference
proceedings 8 : pp 1693 – 1697.
[6] Uba S; Uzairu A, Harrison G.F.S, Balarabe
M.L and Okunola O.J (2008) Assessment of
heavy metals bioavailability in dumpsite of
Zaria metropolis Nigeria. African Journal of
Biotechnology 7(2) 122 – 130.
[7] Zaku S.G, Emmanuel S.A and Thomas S.A
(2011).Assessing the level of soil nutrient: a
case study of Donga,Ibi and Wukari
farmlands in Taraba State, Nigeria,
Agric.Biol.J.N. Am., 2(1) : 101 – 108.
[8] Zampella M., (2003): Characterization of
heavy metals in contaminated soils of the
solofrana river valley South Italy Geoderma
117, 347 – 366.

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Be4301314318

  • 1. M Imam Mohammed et al Int. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 3( Version 1), March 2014, pp.314-318 www.ijera.com 314 | P a g e Effect of Electrical Conductivity on the Soil of Irrigated Farmlands of Kaduna Metropolis Nigeria W.L.O Jimoh1 and Mahmud Imam Mohammed2 1 Department of Pure and Industrial Chemistry, Bayero University, Kano Nigeria. 2 Department of Applied Science, College of Science and Technology, Kaduna Polytechnic ABSTRACT The objective of this research work is to assess the level of electrical conductivity in the soil of irrigated farmlands of Kaduna metropolis using conductivity meter. It was found that lowest electrical conductivity of 1.14 µScm-1 was obtained from Badiko samples and the highest from Kawo with conductivity of 2.63 µScm-1 . It was also found that from the ANOVA p = 0.000<0.05 shows that there is significant differences in the electrical conductivity of soil across the various sampling sites. The real differences of soil conductivity was further analyzed by a post-hoc test using the Duncan Multiple range test with samples from Badiko and Nasarawa having the least soil conductivity. In the second homogeneous subgroup there is Danmani, Abakpa, Makera, Doka etc. The third subgroup include Rigasa, Kabala, Barnawa,Kakuri, Kawo, Malali while the highest soil conductivity fall in the fourth subgroup which include Kawo and Rigachikun (control sites). Infact most of the samples were moderately saline while some are non saline, as a result of human activities occurring in such sites, hence, increase the mobility of heavy metals in the soil. Thereby leading to the toxicity and polluting the soil as well as reducing its ability in the production of crops and vegetables in the affected agricultural areas. Keywords: Soil, conductivity Meter, Kaduna Metropolis, Nigeria. I. INTRODUCTION Electrical conductivity (EC) is the ability of a material to transmit (conduct) an electrical current and is commonly expressed in units of milliSiemens per meter (mS/m). Soil electrical (EC) is a measurement that correlates with soil properties that affect crop productivity, including soil texture, cation exchange capacity (CEC), drainage conditions, organic matter level, salanity and subsoil characteristic The electrical conductivity of soil varies depending on the amount of moisture held by soil particles. Sands have a low conductivity, silts have a medium conductivity and clays have a high conductivity. Soil electrical conductivity (EC) can be related to specific soil properties that affect crop yield such as topsoil depth, PH, salt concentrations and available water – holding capacity. Soil is a dynamic layer in which many chemicals, physical and biological activities are going on constantly. It is not a lifeless zone but an active system having inputs and outputs of energy and matter. The soil has become adjusted to a prevailing condition of climate and plant cover may change when the prevailing condition change (Ademoroti, 1996). Irrigation is the artificial means of water supply to the agricultural crops ranging from surface irrigation, micro sprayer and low-head barber irrigation. Irrigation is design to permit farming in arid regions and offset drought in semi-arid or semi humid regions. The type of irrigation system employed in the farmlands of the Kaduna metropolis is the surface irrigation where water is applied directly to the soil surface through channel which varies in size from individual furrow to large basin. Domestic waste water contains metal from metabolic waste, corrosion of water pipes and consumer products. Industrial effluents and water slug may substantially contribute to the metal loading (Zapella, 2003). In Nigeria the use of polluted water in the immediate surroundings of big cities for growing of vegetables is a common practice. Although this water is considered to be rich source of organic matter and plant nutrients, it also contains sufficient amounts of soluble salts and heavy metals like Fe, Mn, Cu, Zn, Pb, etc. When such water is used for cultivation of crops for a long period, heavy metals may accumulate in soil and may be toxic to the plants. (Kirkhan, 1983). Long term waste water irrigation may lead to the accumulation of heavy metals in agricultural soils and plants. Food safety issues and potential health risks make this as one of the most serious environment concerns (Cui et al., 2004). Consequently, with the increasing use of fertilizers, RESEARCH ARTICLE OPEN ACCESS
  • 2. M Imam Mohammed et al Int. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 3( Version 1), March 2014, pp.314-318 www.ijera.com 315 | P a g e biosolid and other related amendments to boost agricultural production and increasing reuse of treated and untreated wastewater as irrigation water, especially in the developing regions of the world, there is need to adequately assess the possible environmental impacts of such applications and agricultural practices.(Tijani and Agakwu) The aim of this research work is to assess the effect of electrical conductivity on the soils used as agricultural areas of Kaduna metropolis so as to ascertain the extent of its pollution. II. MATERIAL AND METHOD Sample and Sampling: Soil samples were randomly collected in a hole of 10cm deep which was dug from the irrigated farmlands where vegetables were grown and irrigated with water. These samples were then stored in polythene bags and taken to the laboratory and dried in an oven at a temperature of 1050 C. The dried soil samples were ground with mortar and pestle and sieved with 2mm sieve. III. DESCRIPTION OF THE SAMPLING SITES Soil samples for heavy metal determination were collected from twenty one (21) irrigation sites of the Kaduna metropolis. These sites were Kabala (KBL), Danmani (DMN), Rigasa (RGS), Barnawa (BNW), Makera (MKR), Kakuri (KKR), Badiko (BDK) Nasarawa (NAS, Malali (MAL), Kudenda (KUD), Kinkinau (KKN), Kawo (KWO), Unguwan Rimi (URM), Unguwan Sanusi (UNS), Tudun Wada (TDW), Doka (DKA), Unguwan Dosa (UDS), Kabala Costain (CTA), Kurmin Mashi (KMS) and Abakpa (ABK). In this research work soil sample from Rigachikun (RCK) irrigation site was taken as control site. Figure 1.0 shows the detail map of the sampling sites. Fig 1.0 Map of the Sampling points and the control site SAMPLE PREPARATION Determination of conductivity 20g of the ground soil sample was taken into a beaker and 100cm3 of distilled water was added and mixed thoroughly. The sample was allowed to stand for 10 minutes. The sample solution was then decanted into another clean beaker. The conductivity meter of the sample solutions were determined using a model ELE 470 conductivity metre. This conductivity metre was turned on and the probe was inserted into the decanted suspended solution of soil samples. The conductivity of each solution was taken and recorded. The probe was removed from the samples and thoroughly rinsed with distilled water. The procedure was repeated for all the samples collected from the various farmlands in the present study. IV. RESULTS AND DISCUSSION The mean conductivity of the soil from the various irrigation sites of the Kaduna metropolis are summarized in the below Table 1.0. Fig 1.0: Distribution of conductivity in soil from different sites of the Kaduna metropolis. 95% Confidence Interval for Mean Lower Bound Upper Bound SL (KBL) 1.793 0.301 0.174 1.045 2.541 SL (DMN) 1.570 0.044 0.025 1.462 1.678 SL (RGS) 1.760 0.052 0.030 1.631 1.889 SL (BNW) 1.827 0.237 0.137 1.238 2.415 SL (MKR) 1.720 0.017 0.010 1.677 1.763 SL (KKR) 1.990 0.060 0.035 1.841 2.139 SL (BDK) 1.138 0.844 0.488 0.960 3.235 SL (NAS) 1.470 0.070 0.040 1.296 1.644 SL (MAL) 2.537 0.474 0.273 1.360 3.713 SL (KKR) 1.960 0.442 0.255 0.861 3.059 SL (KKN) 2.297 0.614 0.355 0.771 3.822 SL (KWO) 2.633 0.754 0.435 0.760 4.506 SL (URM) 2.260 0.862 0.497 0.120 4.400
  • 3. M Imam Mohammed et al Int. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 3( Version 1), March 2014, pp.314-318 www.ijera.com 316 | P a g e SL (UNS) 2.343 0.560 0.323 0.952 3.735 SL (TDW) 2.453 0.912 0.527 0.187 4.719 SL (DKA) 1.723 0.059 0.034 1.578 1.869 SL (UNS) 1.610 0.036 0.021 1.520 1.700 SL (CTA) 2.110 0.235 0.136 1.526 2.694 SL (KMS) 1.723 0.211 0.122 1.200 2.247 SL (ABK) 1.620 0.062 0.036 1.465 1.775 SL RCK (Control) 2.643 0.625 0.361 1.092 4.195 Table 1.0 shows the electronic conductivity soil samples obtained from the 21 irrigation sampling sites of the Kaduna metropolis. Conductivity of the Soil Samples The electrical conductivity of the soil samples from the irrigation sites indicated the lowest conductivity of 1.14 µScm-1 from Badiko sample and highest from Kawo with conductivity of 2.63 µScm-1 and were both lower than the conductivity value of 3.00µScm_1 obtained in soil from Zaria 3.00µscm-1 ( Uba et al.,2008). The higher conductivity value of the soil obtained from Zaria when compared to that obtained in this work may be attributed to the presence of certain element such as Na,Ca,Mg,K,Fe,Cu Zn etc were constituent of the soil and were abundance in the former than in the later. Table2.0: ANOVA Table for Conductivity Source of Variation Sum of Squares DF Mean Square F Sig. Between Groups 10.295 20 0.515 2.337 0.010 Within Groups 9.250 42 0.220 Total 19.545 62 From the ANOVA table 2.0 above, 05.0010.0 p there is significant difference in the conductivity across the various sample sites. The real differences of conductivity further be analyzed by a post-hoc test using the Duncan Multiple range test in the table below; where means of homogeneous subgroups are clearly displayed. Moreover, the mean plots that follow clearly depict the mean values of the conductivity across the various locations. Table 3.0: Duncan Test for Conductivity Subset for alpha = 0.05 1 2 3 4 Badiko 1.14 Nasarawa 1.47 Danmani 1.57 Unguwan Dosa 1.61 Abakpa 1.62 Makera 1.72 Doka 1.72 Kurmin Mashi 1.72 Rigasa 1.76 Kabala 1.79 Barnawa 1.83 Kudenda 1.96
  • 4. M Imam Mohammed et al Int. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 3( Version 1), March 2014, pp.314-318 www.ijera.com 317 | P a g e Kakuri 1.99 Costain 2.11 Unguwan Rimi 2.26 Kinkinau 2.30 Unguwan Sanusi 2.34 Tudun Wada 2.45 Malali 2.54 Kawo 2.63 Rigachikun (Control) 2.64 Sig. 0.070 0.066 0.063 0.051 From the Duncan multiple range tests displayed in Table 3.0, Badiko and Nasarawa, have the least conductivity. In the second homogeneous subgroup we have Danmani, Unguwan Dosa, Abakpa, among others. Similarly, in the third homogeneous subgroup we have Rigasa, Kabala, Barnawa, among others. The highest conductivity fall in the fourth subgroup; which include only Kawo and Rigachikun. This is depicted in figure 2.0 0 0.5 1 1.5 2 2.5 3 BadikoN asaraw a D anm ani U nguw an D osa Abakpa M akera D oka Kurm in M ashi R igasa Kabala Barnaw aKudenda Kakuri C ostain U nguw an R im iKinkinau U nguw an Sanusi Tudun W ada M alali Kaw o R igachikun (C ontrol) Sampling Site Meanconductivity(uS/cm) Series1 Series2 Series3 Series4 Fig.2.0: A mean Plot for Conductivity However, all conductivity values of the analyzed soil in this research work were within the normal range ,that is, 0 - 200µscm-1 as reported by Zaku et al., (2011). The soil electrical conductivity varies significantly from one farmland to another (p < 0.005). Boulding (1994) classified electrical conductivity of soil as non – saline < 2; moderately saline 2 – 8; very saline 8 – 16 ; extremely saline >16. From the result of this research work, most of the samples were moderately saline while some are non saline, as a result of human activities occurring in such sites . Hence, increase the mobility heavy metals in the soil. V. CONCLUSION In the present study, the electrical conductivity of different irrigation sites of Kaduna metropolis were determined and found that most of these sites were within the normal range ,that is, 0 - 200µscm-1 as reported by Zaku et al., (2011). Also
  • 5. M Imam Mohammed et al Int. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 3( Version 1), March 2014, pp.314-318 www.ijera.com 318 | P a g e most of the samples were moderately saline while some are non saline, as a result of human activities occurring in such sites. Hence, increase the mobility of heavy metals in the soil. Thereby leading to toxicity and polluting the soil as well as reducing its ability in the production of crops and vegetables in the affected agricultural areas.. VI. ACKNOWLEDGEMENT The Authors were grateful to the management of Kaduna Polytechnic for sponsoring this research work. REFERENCES [1] Ademoroti C.M.A (1996): Soil, water and air environmental chemistry and texiocology. Foludex Press Ibadan, 1st Edition Pp 30-34. [2] Boulding, J. R (1994). Description and sampling of contaminated soils. Alfeid Guide. 2nd Edn. Lewis publishers, Boca Raton, FL. Pp 5 [3] Cui, Y.J, Zhu, Y.G, Zhain R.H, Chen, D.Y, Huang Y.Z, Qui Y and Liang J.Z (2004). Tranfer of metals from nrar a smelter in Nanning., China. Environmental International 30: 785 – 791. [4] Kirkhan, M.B (1983), study on accumulation of heavy metals in soil receiving sewage and effluent water. Agric. Ecosystem, Environment 9:251. [5] Tijani, M.N and Agakwu, A.A (2007) An assessment of soil – plant transfer of trace metals and contamination of shallow groundwater under amendment irrigated fields. African crop science conference proceedings 8 : pp 1693 – 1697. [6] Uba S; Uzairu A, Harrison G.F.S, Balarabe M.L and Okunola O.J (2008) Assessment of heavy metals bioavailability in dumpsite of Zaria metropolis Nigeria. African Journal of Biotechnology 7(2) 122 – 130. [7] Zaku S.G, Emmanuel S.A and Thomas S.A (2011).Assessing the level of soil nutrient: a case study of Donga,Ibi and Wukari farmlands in Taraba State, Nigeria, Agric.Biol.J.N. Am., 2(1) : 101 – 108. [8] Zampella M., (2003): Characterization of heavy metals in contaminated soils of the solofrana river valley South Italy Geoderma 117, 347 – 366.