ESTIMATION OF THE EFFECT OF IRRIGATION ON ANNUAL RECHARGE AT THE KANO PROJECT AREA OF KANO RIVER BASIN
ESTIMATION OF THE EFFECT OF IRRIGATION ON ANNUAL RECHARGE AT THE KANO PROJECT AREA OF KANO RIVER BASIN
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Date
1991-12
Authors
DAURA, HUSSAINI AHMED
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Abstract
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
This study was carried out to investigate and quantify
the effect of irrigation on annual recharge at the Kano
project area of Kano river Project. The soil moisture
deficit model was used in estimating the recharge and its
sensitivity to data and model parameters was investigated.
The mean annual recharge for the whole area was
estimated at 101.1 mm. In the irrigated areas, the mean
annual recharge was 262.1 mm, out of which an average
17 2.6 mm comes from irrigation.
The sensitivity analysis has shown the model to be
sensitive to variations in rainfall and potential
evapotranspiration.
Description
A THESIS SUBMITTED TO THE POSTGRADUATE SCHOOL,
AHMADU BELLO UNIVERSITY, IN PARTIAL FULFILLMENT
OF THE REQUIREMENTS FOR THE DEGREE OF
MASTER OF ENGINEERING IN
WATER RESOURCES AND ENVIROMENTAL ENGINEERING
DEPARTMENT OF WATER RESOURCES AND ENVIROMENTAL ENGINEERING
FACULTY OF ENGINEERING
AHMADU BELLO UNIVERSITY
ZARIA, NIGERIA
DECEMBER, 1991
A THESIS SUBMITTED TO THE POSTGRADUATE SCHOOL,
AHMADU BELLO UNIVERSITY, IN PARTIAL FULFILLMENT
OF THE REQUIREMENTS FOR THE DEGREE OF
MASTER OF ENGINEERING IN
WATER RESOURCES AND ENVIROMENTAL ENGINEERING
DEPARTMENT OF WATER RESOURCES AND ENVIROMENTAL ENGINEERING
FACULTY OF ENGINEERING
AHMADU BELLO UNIVERSITY
ZARIA, NIGERIA
DECEMBER, 1991
A THESIS SUBMITTED TO THE POSTGRADUATE SCHOOL,
AHMADU BELLO UNIVERSITY, IN PARTIAL FULFILLMENT
OF THE REQUIREMENTS FOR THE DEGREE OF
MASTER OF ENGINEERING IN
WATER RESOURCES AND ENVIROMENTAL ENGINEERING
DEPARTMENT OF WATER RESOURCES AND ENVIROMENTAL ENGINEERING
FACULTY OF ENGINEERING
AHMADU BELLO UNIVERSITY
ZARIA, NIGERIA
DECEMBER, 1991
A THESIS SUBMITTED TO THE POSTGRADUATE SCHOOL,
AHMADU BELLO UNIVERSITY, IN PARTIAL FULFILLMENT
OF THE REQUIREMENTS FOR THE DEGREE OF
MASTER OF ENGINEERING IN
WATER RESOURCES AND ENVIROMENTAL ENGINEERING
DEPARTMENT OF WATER RESOURCES AND ENVIROMENTAL ENGINEERING
FACULTY OF ENGINEERING
AHMADU BELLO UNIVERSITY
ZARIA, NIGERIA
Keywords
ESTIMATION, EFFECT, IRRIGATION, IANNUAL, RECHARGE, PROJECT, KANO