Pedo-Transfer Function of Paddy Soils Saturated Hydraulic Conductivity

 
9783847346524: Pedo-Transfer Function of Paddy Soils Saturated Hydraulic Conductivity
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Soil saturated hydraulic conductivity (Ks) is an important soil physical property, especially for determining infiltration rate, irrigation practice, drainage design, run off, deep percolation, groundwater recharge and in simulating leaching and other agricultural and hydrological processes. Several laboratory and field methods can be used to determine Ks. Unfortunately, laboratory and field determinations are usually time consuming, expensive and labour intensive. This study attempts to simplify the determination of Ks. The main objectives of this study were to seek a simplified method for determining Ks values based on PTF and estimate DP losses in paddy field based on the dominant Ks of the soil profile.

Biografía del autor:

Dr Aimrun Wayayok (Soil and Water Engineering, Precision Farming Engineering)is a fellow researcher at Universiti Putra Malaysia.He was born in Patani, Thailand on 20th August 1977. He has published for about 100 articles in various kinds of publication such as peer reviewed journals,conference proceedings and chapter in books.

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Descripción Condición: New. Publisher/Verlag: LAP Lambert Academic Publishing | A simplified method for determining Ks values | Soil saturated hydraulic conductivity (Ks) is an important soil physical property, especially for determining infiltration rate, irrigation practice, drainage design, run off, deep percolation, groundwater recharge and in simulating leaching and other agricultural and hydrological processes. Several laboratory and field methods can be used to determine Ks. Unfortunately, laboratory and field determinations are usually time consuming, expensive and labour intensive. This study attempts to simplify the determination of Ks. The main objectives of this study were to seek a simplified method for determining Ks values based on PTF and estimate DP losses in paddy field based on the dominant Ks of the soil profile. | Format: Paperback | Language/Sprache: english | 192 pp. Nº de ref. del artículo: K9783847346524

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Descripción LAP Lambert Academic Publishing Jan 2012, 2012. Taschenbuch. Condición: Neu. Neuware - Soil saturated hydraulic conductivity (Ks) is an important soil physical property, especially for determining infiltration rate, irrigation practice, drainage design, run off, deep percolation, groundwater recharge and in simulating leaching and other agricultural and hydrological processes. Several laboratory and field methods can be used to determine Ks. Unfortunately, laboratory and field determinations are usually time consuming, expensive and labour intensive. This study attempts to simplify the determination of Ks. The main objectives of this study were to seek a simplified method for determining Ks values based on PTF and estimate DP losses in paddy field based on the dominant Ks of the soil profile. 192 pp. Englisch. Nº de ref. del artículo: 9783847346524

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Aimrun Wayayok
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Descripción LAP Lambert Academic Publishing Jan 2012, 2012. Taschenbuch. Condición: Neu. Neuware - Soil saturated hydraulic conductivity (Ks) is an important soil physical property, especially for determining infiltration rate, irrigation practice, drainage design, run off, deep percolation, groundwater recharge and in simulating leaching and other agricultural and hydrological processes. Several laboratory and field methods can be used to determine Ks. Unfortunately, laboratory and field determinations are usually time consuming, expensive and labour intensive. This study attempts to simplify the determination of Ks. The main objectives of this study were to seek a simplified method for determining Ks values based on PTF and estimate DP losses in paddy field based on the dominant Ks of the soil profile. 192 pp. Englisch. Nº de ref. del artículo: 9783847346524

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Descripción LAP Lambert Academic Publishing Jan 2012, 2012. Taschenbuch. Condición: Neu. This item is printed on demand - Print on Demand Neuware - Soil saturated hydraulic conductivity (Ks) is an important soil physical property, especially for determining infiltration rate, irrigation practice, drainage design, run off, deep percolation, groundwater recharge and in simulating leaching and other agricultural and hydrological processes. Several laboratory and field methods can be used to determine Ks. Unfortunately, laboratory and field determinations are usually time consuming, expensive and labour intensive. This study attempts to simplify the determination of Ks. The main objectives of this study were to seek a simplified method for determining Ks values based on PTF and estimate DP losses in paddy field based on the dominant Ks of the soil profile. 192 pp. Englisch. Nº de ref. del artículo: 9783847346524

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Aimrun Wayayok
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Descripción LAP Lambert Academic Publishing. Paperback. Condición: New. 192 pages. Dimensions: 8.7in. x 5.9in. x 0.4in.Soil saturated hydraulic conductivity (Ks) is an important soil physical property, especially for determining infiltration rate, irrigation practice, drainage design, run off, deep percolation, groundwater recharge and in simulating leaching and other agricultural and hydrological processes. Several laboratory and field methods can be used to determine Ks. Unfortunately, laboratory and field determinations are usually time consuming, expensive and labour intensive. This study attempts to simplify the determination of Ks. The main objectives of this study were to seek a simplified method for determining Ks values based on PTF and estimate DP losses in paddy field based on the dominant Ks of the soil profile. This item ships from multiple locations. Your book may arrive from Roseburg,OR, La Vergne,TN. Paperback. Nº de ref. del artículo: 9783847346524

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