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發(fā)表于 2025-3-21 18:51:56 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Groundwater Recharge from Run-off, Infiltration and Percolation
編輯K.-P. Seiler,J.R. Gat
視頻videohttp://file.papertrans.cn/389/388862/388862.mp4
叢書名稱Water Science and Technology Library
圖書封面Titlebook: ;
出版日期Book 2007
版次1
doihttps://doi.org/10.1007/978-1-4020-5306-1
isbn_softcover978-90-481-7333-4
isbn_ebook978-1-4020-5306-1Series ISSN 0921-092X Series E-ISSN 1872-4663
issn_series 0921-092X
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 20:24:02 | 只看該作者
板凳
發(fā)表于 2025-3-22 00:55:52 | 只看該作者
Michele Torre,Marcello Carlucci, it must be clarified to which extent the studied hydro-geologic system discharges under steady-state respectively transient hydraulic conditions; both conditions occur naturally world wide, because of the always existing global changes in climates, vegetation, and discharge levels (chapter 1), whi
地板
發(fā)表于 2025-3-22 05:05:29 | 只看該作者
5#
發(fā)表于 2025-3-22 09:06:48 | 只看該作者
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發(fā)表于 2025-3-22 14:14:17 | 只看該作者
Research Tools and Methods in the Study of Recharge,, it must be clarified to which extent the studied hydro-geologic system discharges under steady-state respectively transient hydraulic conditions; both conditions occur naturally world wide, because of the always existing global changes in climates, vegetation, and discharge levels (chapter 1), whi
7#
發(fā)表于 2025-3-22 19:09:26 | 只看該作者
Thoracic Trauma. General ConsiderationsThe groundwater recharge flux is the residuum of the infiltration flux after accounting for water storage, losses by evapo-transpiration and of inter-flow in the percolation zone; it enters groundwater through the capillary fringe and the groundwater table.
8#
發(fā)表于 2025-3-23 00:08:05 | 只看該作者
Diagnostic Techniques in the EsophagusThis general scheme is modified by the plant cover, land/water partitioning, ocean currents and topographic features (section 2.2.2). Such climate zones, however, are responsible for the different contribution of precipitation to run-off generation and the groundwater recharge.
9#
發(fā)表于 2025-3-23 04:42:38 | 只看該作者
Tara Loux,Christopher P. CoppolaThe water cycle is being constantly and slowly modified since ever by atmospheric, erosion, land cover, and tectonic changes; these changes have been accelerated since activities and growth of mankind (Fig. 6.1) passed a certain threshold number in about the year 1850.
10#
發(fā)表于 2025-3-23 06:35:54 | 只看該作者
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