Water movement in a conditioner-treated sandy soil in Saudi Arabia

1994 ◽  
Vol 27 (4) ◽  
pp. 363-373 ◽  
Author(s):  
R.E.A. Sabrah
Keyword(s):  
Saudi Arabia ◽  
Sandy Soil ◽  
Water Movement

scholarly journals Effects of biochar on water movement characteristics in sandy soil under drip irrigation

2019 ◽  
Vol 11 (5) ◽  
pp. 740-753
Author(s):  
Shenghai Pu ◽  
Guangyong Li ◽  
Guangmu Tang ◽  
Yunshu Zhang ◽  
Wanli Xu ◽  
...  
Keyword(s):  
Sandy Soil ◽  
Drip Irrigation ◽  
Water Movement ◽  
Movement Characteristics

Characteristics and productivity of a sandy soil as influenced by soil conditioners in Saudi Arabia

1993 ◽  
Vol 24 (3) ◽  
pp. 297-304 ◽  
Author(s):  
R.E.A. Sabrah ◽  
M.F. Ghoneim ◽  
H.M. Abd El-Magid ◽  
R.K. Rabie
Keyword(s):  
Saudi Arabia ◽  
Sandy Soil ◽  
Soil Conditioners

Improvement of Water Movement in an Undulating Sandy Soil Prone to Water Repellency

2011 ◽  
Vol 10 (1) ◽  
pp. 262-269 ◽  
Author(s):  
Klaas Oostindie ◽  
Louis W. Dekker ◽  
Jan G. Wesseling ◽  
Coen J. Ritsema
Keyword(s):  
Sandy Soil ◽  
Water Movement ◽  
Water Repellency

Optimizing physical properties of a sandy soil for higherproductivity using town refuse compost in Saudi Arabia

1995 ◽  
Vol 29 (2) ◽  
pp. 253-262 ◽  
Author(s):  
Ragaá E.A. Sabrah ◽  
Hago M. Abdel Magid ◽  
Shafik I. Abdel-Aal ◽  
Rafaát K. Rabie
Keyword(s):  
Saudi Arabia ◽  
Physical Properties ◽  
Sandy Soil

Phosphorus forms in a sandy soil (Torripsamment) under palm orchards of different age in Saudi Arabia

1995 ◽  
Vol 46 (3) ◽  
pp. 481-488 ◽  
Author(s):  
M.S. HEAKAL ◽  
M.H. AL-AWAJY ◽  
M.S. AL-SEWAILEM ◽  
F.N. BARAKAH ◽  
A. AL-ASHEIKH
Keyword(s):  
Saudi Arabia ◽  
Sandy Soil ◽  
Phosphorus Forms

scholarly journals Impact of Sewage Sludge on Water Movement in Calcareous Sandy Soils

1997 ◽  
Vol 2 ◽  
pp. 59
Author(s):  
A.M. AI-Omran ◽  
M.I. AI-Wabel ◽  
A.A. Shalaby
Keyword(s):  
Sewage Sludge ◽  
Sandy Soil ◽  
Water Movement ◽  
Soil Depth ◽  
Sandy Soils ◽  
Water Diffusivity ◽  
Caco3 Content ◽  
Cumulative Infiltration ◽  
Exponential Decrease ◽  
Disturbed Soils

The present study was undertaken to investigate the changes in soil physical properties and their effect on water movement under ponded irrigation. Sewage sludge was applied to 10 cm soil depth at rates of 0.25. 75  and 100 Mg-ha-1 to two disturbed soils differing in CaCO3 content. The results showed that cumulative infiltration (1) decreased with an increase in sewage sludge rates. Basic infiltration for slightly calcareous sandy soil was higher than that of moderately calcareous sandy soil, laboratory measurements showed an exponential decrease in saturated hydraulic conductivity and an increase in available water capacity with an increase in sewage sludge rates. For both soils, water diffusivity (D(Q)) decreased with an increase in sewage sludge rates. The (oral) values of slightly calcareous sandy soils were higher than those of moderately calcareous sandy soils.

Qualitative Sensing of Water Movement from a Point-source Emitter on a Sandy Soil

1993 ◽  
Vol 9 (3) ◽  
pp. 299-303 ◽  
Author(s):  
G. A. Clark ◽  
C. D. Stanley ◽  
F. S. Zazueta
Keyword(s):  
Point Source ◽  
Sandy Soil ◽  
Water Movement

Impact of Natural Clay Deposits on Water Movement in Calcareous Sandy Soil

2002 ◽  
Vol 16 (2) ◽  
pp. 185-193 ◽  
Author(s):  
A. M. Al-Omran ◽  
M. I. Choudhary ◽  
A. A. Shalaby ◽  
M. M. Mursi
Keyword(s):  
Sandy Soil ◽  
Water Movement ◽  
Natural Clay ◽  
Clay Deposits
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