000			018790000a22003370004500
003			EG-GICUC
005			20250223031651.0
008			070224s2006 ua d f m 000 0 Eng d
040			_aEG-GICUC _beng _cEG-GICUC
041	0		_aEng
049			_aDeposite
097			_aM.Sc
099			_aCai01.13.05.M.Sc.2006.Ya.A
100	0		_aYasser Nasser Aljabry
245	1	0	_aArtificial recharge in shallow water table aquifers / _cYasser Nasser Aljabry ; Supervised Alaa Aldain Alzawahry , Ahmed Wagdy Abdaldaim , Emad Yousef Nessem
246	1	5	_aالتغذية الصناعية للاحواض الجوفية غير العميقة
260			_aCairo : _bYasser Nasser Aljabry , _c2006
300			_a119p : _bcharts ; _c30cm
502			_aThesis (M.Sc.) - Cairo University - Faculty Of Engineering - Department Of Civil Engineering
520			_aInfiltration 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
530			_aIssued also as CD
653		4	_aArtificial
653		4	_ashallow water table
700	0		_aAhmed Wagdy Abdaldaim , _eSupervisor
700	0		_aAlaa Aldain Alzawahry , _eSupervisor
700	0		_aEmad Yousef Nessem , _eSupervisor
856			_uhttp://172.23.153.220/th.pdf
905			_aAml _eCataloger
905			_aEsam _eRevisor
942			_2ddc _cTH
999			_c59877 _d59877