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Artificial recharge in shallow water table aquifers / Yasser Nasser Aljabry ; Supervised Alaa Aldain Alzawahry , Ahmed Wagdy Abdaldaim , Emad Yousef Nessem

By: Contributor(s): Language: Eng Publication details: Cairo : Yasser Nasser Aljabry , 2006Description: 119p : charts ; 30cmOther title:
  • التغذية الصناعية للاحواض الجوفية غير العميقة [Added title page title]
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  • Issued also as CD
Dissertation note: Thesis (M.Sc.) - Cairo University - Faculty Of Engineering - Department Of Civil Engineering Summary: Infiltration is the process by which water on the ground surface enters the soil Infiltration is governed by two forces , gravity , and capillary action While smaller pores offer greater resistance to gravity , very small pores pull water through capillary action in addition to and even against the force of gravity The rate of infiltration is affected by soil characteristics including ease of entry , storage capacity , and transmission rate through the soil The soil texture and structure , vegetation types and cover , water content of the soil , soil temperature , and rainfall intensity all play a role in dictating infiltration rate and capacity
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Thesis Thesis قاعة الرسائل الجامعية - الدور الاول المكتبة المركزبة الجديدة - جامعة القاهرة Cai01.13.05.M.Sc.2006.Ya.A (Browse shelf(Opens below)) Not for loan 01010110046609000
CD - Rom CD - Rom مخـــزن الرســائل الجـــامعية - البدروم المكتبة المركزبة الجديدة - جامعة القاهرة Cai01.13.05.M.Sc.2006.Ya.A (Browse shelf(Opens below)) 46609.CD Not for loan 01020110046609000

Thesis (M.Sc.) - Cairo University - Faculty Of Engineering - Department Of Civil Engineering

Infiltration is the process by which water on the ground surface enters the soil Infiltration is governed by two forces , gravity , and capillary action While smaller pores offer greater resistance to gravity , very small pores pull water through capillary action in addition to and even against the force of gravity The rate of infiltration is affected by soil characteristics including ease of entry , storage capacity , and transmission rate through the soil The soil texture and structure , vegetation types and cover , water content of the soil , soil temperature , and rainfall intensity all play a role in dictating infiltration rate and capacity

Issued also as CD

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