標(biāo)題: Titlebook: Estimation of Natural Groundwater Recharge; Ian Simmers (Director) Book 1988 Springer Science+Business Media Dordrecht 1988 Arid Zone.Prec [打印本頁(yè)] 作者: fundoplication 時(shí)間: 2025-3-21 19:19
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書目名稱Estimation of Natural Groundwater Recharge讀者反饋
書目名稱Estimation of Natural Groundwater Recharge讀者反饋學(xué)科排名
作者: Kidnap 時(shí)間: 2025-3-21 22:33
An Unexpected Factor Affecting Recharge from Ephemeral River Flows in SWA/Namibia. Casual observations in ephemeral rivers in SWA/Namibia have indicated that variable recharge quantities result from similar flood events. For this reason the Department of Water Affairs initiated a research project to identify and investigate relevant parameters. To achieve these objectives three 作者: Classify 時(shí)間: 2025-3-22 01:57 作者: Unsaturated-Fat 時(shí)間: 2025-3-22 07:46
A Review of Some of the Physical, Chemical and Isotopic Techniques Available for Estimating Groundwasents a loss in yield and so should be minimised. Those who are interested in water resources, take the opposite view. A few of the reasons for studying natural groundwater recharge are: to determine the safe yield of a groundwater system; to assess the extent of development of secondary salinisatio作者: malign 時(shí)間: 2025-3-22 10:43
Evaporation in Arid and Semi-Arid Regionssed..It is pointed out that most models for evaporation are developed for temperate crops. The main differences between temperate and (semi-)arid regions are described..Special attention will be paid to the use of remote sensing techniques, for the determination of evaporation.作者: 驚呼 時(shí)間: 2025-3-22 16:19 作者: 驚呼 時(shí)間: 2025-3-22 18:37
A Proposed Study of Recharge Processes in Fracture Aquifers of Semi-Arid Botswanahe evapotranspiration and the groundwater discharge component are not directly measurable. Moreover, the storage of moisture in the unsaturated zone and the rates of infiltration along the various possible routes to the aquifer form important and uncertain factors. Linked in with plans to extend and作者: BOOR 時(shí)間: 2025-3-23 01:03 作者: condemn 時(shí)間: 2025-3-23 04:19 作者: ARY 時(shí)間: 2025-3-23 08:02 作者: dagger 時(shí)間: 2025-3-23 10:42 作者: 愚蠢人 時(shí)間: 2025-3-23 14:09
Comparison of Recharge Estimates from Injected Tritium Technique and Regional Hydrological Modellingsub-basin, forming a part of the Vedavati basin and having an area of 958 Sq. Km., covered with granite, gneisses, and schists. Recharge was measured at 20 sites, of which 6 were in schists and the rest in gneisses. Displacement of Tritium tracer peak in the unsaturated Alfisol zone was used for mea作者: 折磨 時(shí)間: 2025-3-23 18:18 作者: Fecal-Impaction 時(shí)間: 2025-3-23 22:30 作者: 燕麥 時(shí)間: 2025-3-24 06:09 作者: BRIDE 時(shí)間: 2025-3-24 09:10
The Principles of Inverse Modelling for Estimation of Recharge from Hydraulic Headsivity functions. The obstacles for doing this are as follows. Taking derivatives of the spatially-distributed data, even when they are known at every point, leads to numerical instability. Hydraulic heads are always measured with inaccuracies. Differentiating this “noisy” data leads to large errors作者: monochromatic 時(shí)間: 2025-3-24 12:57
1389-2185 evelopments relating to natural recharge indicate the following ‘problems‘ ; no single comprehensive estimation technique can yet be iden- tified from the spect978-90-481-8444-6978-94-015-7780-9Series ISSN 1389-2185 作者: 四目在模仿 時(shí)間: 2025-3-24 16:29 作者: photophobia 時(shí)間: 2025-3-24 22:39 作者: Decimate 時(shí)間: 2025-3-25 02:01 作者: 善變 時(shí)間: 2025-3-25 03:20
Solute Profile Techniques for Recharge Estimation in Semi-Arid and Arid Terrainive tool for estimating direct recharge in porous lithologies of semi-arid regions and also for investigating recharge history, providing input data for chloride are available. In more arid regions, however, a component of discharge may occur during hyperarid episodes. Further validation of moisture作者: 希望 時(shí)間: 2025-3-25 07:53 作者: 小臼 時(shí)間: 2025-3-25 13:40 作者: sultry 時(shí)間: 2025-3-25 16:05
Comparison of Recharge Estimates from Injected Tritium Technique and Regional Hydrological Modelling fluctuation data for the period November 1977 to November 1978, these authors have estimated the annual recharge for various parts of the Vedavati basin. The annual recharge or safe yield value for West-Survarnamukhi basin, obtainable from the model, is 42.5 mm. Thus, an agreement between recharge 作者: 潛移默化 時(shí)間: 2025-3-25 20:17
Methods for Estimation of Natural Groundwater Recharge Directly from Precipitation — Comparative Stuements and a catchment area model, calibrated against them, gave valuable information of total recharge quantities, which could be used for comparisons with the other methods..The study clearly demonstrated the need for comparative studies with several methods, since all estimations suffered from su作者: hurricane 時(shí)間: 2025-3-26 02:54 作者: 展覽 時(shí)間: 2025-3-26 07:18 作者: cutlery 時(shí)間: 2025-3-26 09:14
https://doi.org/10.1057/9781137008565ive tool for estimating direct recharge in porous lithologies of semi-arid regions and also for investigating recharge history, providing input data for chloride are available. In more arid regions, however, a component of discharge may occur during hyperarid episodes. Further validation of moisture作者: senile-dementia 時(shí)間: 2025-3-26 16:43 作者: 摘要記錄 時(shí)間: 2025-3-26 20:11 作者: 有限 時(shí)間: 2025-3-27 00:45 作者: 身體萌芽 時(shí)間: 2025-3-27 01:39 作者: peritonitis 時(shí)間: 2025-3-27 06:41
978-90-481-8444-6Springer Science+Business Media Dordrecht 1988作者: 控制 時(shí)間: 2025-3-27 10:34
Estimation of Natural Groundwater Recharge978-94-015-7780-9Series ISSN 1389-2185 作者: 行為 時(shí)間: 2025-3-27 16:30
https://doi.org/10.1007/978-94-015-7780-9Arid Zone; Precipitation; Rain; development; energy; forest; formation; fracture; groundwater; isotope; modeli作者: Ganglion-Cyst 時(shí)間: 2025-3-27 21:25
Nato Science Series C:http://image.papertrans.cn/e/image/315791.jpg作者: painkillers 時(shí)間: 2025-3-27 21:57 作者: chronicle 時(shí)間: 2025-3-28 04:13
https://doi.org/10.1007/BFb0093533. Casual observations in ephemeral rivers in SWA/Namibia have indicated that variable recharge quantities result from similar flood events. For this reason the Department of Water Affairs initiated a research project to identify and investigate relevant parameters. To achieve these objectives three 作者: Genome 時(shí)間: 2025-3-28 06:57
Cassandra Lawrence,Richard J. Tosti aquifer. This hydraulically connected aquifer system is generally regarded as highly discontinuous with individual compartments in which isolated groundwater circulation occurs. Extensive drilling for rural and urban water supply in Burkina Faso, Niger and Ghana has, however, brought evidence for t作者: 周興旺 時(shí)間: 2025-3-28 13:19
https://doi.org/10.1057/9780230103146sents a loss in yield and so should be minimised. Those who are interested in water resources, take the opposite view. A few of the reasons for studying natural groundwater recharge are: to determine the safe yield of a groundwater system; to assess the extent of development of secondary salinisatio作者: GEON 時(shí)間: 2025-3-28 16:50 作者: 斥責(zé) 時(shí)間: 2025-3-28 21:59 作者: 獨(dú)行者 時(shí)間: 2025-3-29 01:26 作者: 笨拙處理 時(shí)間: 2025-3-29 06:40 作者: cartilage 時(shí)間: 2025-3-29 07:52 作者: 難理解 時(shí)間: 2025-3-29 14:35
Environmental Impacts of Cultivated Meat, chloride in the unsaturated zone. A one-dimensional equation, incorporating convective and diffusion terms, describing steady-state transport of non-reactive solutes, is solved in an inverse fashion, enabling computation of the depth-distribution of vertical water flux density. This and other simpl作者: 故意釣到白楊 時(shí)間: 2025-3-29 17:17 作者: FACT 時(shí)間: 2025-3-29 20:12
Sélim Louafi,Didier Bazile,Jean-Louis Noyersub-basin, forming a part of the Vedavati basin and having an area of 958 Sq. Km., covered with granite, gneisses, and schists. Recharge was measured at 20 sites, of which 6 were in schists and the rest in gneisses. Displacement of Tritium tracer peak in the unsaturated Alfisol zone was used for mea作者: GREG 時(shí)間: 2025-3-30 03:27 作者: etiquette 時(shí)間: 2025-3-30 06:23
Policies, Landscape and Politics estimation of recharge using soil moisture balance models, recharge due to losses from irrigation schemes, the influence of the unsaturated zone and recharge due to rivers and other sources of run-off. A study of the water table fluctuation method indicates that . methods often provide unreliable e作者: Neonatal 時(shí)間: 2025-3-30 10:51 作者: 交響樂(lè) 時(shí)間: 2025-3-30 12:25
Annette Rasmussen,Christian Ydesensivity functions. The obstacles for doing this are as follows. Taking derivatives of the spatially-distributed data, even when they are known at every point, leads to numerical instability. Hydraulic heads are always measured with inaccuracies. Differentiating this “noisy” data leads to large errors作者: Jogging 時(shí)間: 2025-3-30 16:43 作者: 經(jīng)典 時(shí)間: 2025-3-30 20:56
Cullin 3 and Its Role in Tumorigenesis,sed..It is pointed out that most models for evaporation are developed for temperate crops. The main differences between temperate and (semi-)arid regions are described..Special attention will be paid to the use of remote sensing techniques, for the determination of evaporation.作者: Hay-Fever 時(shí)間: 2025-3-31 03:28 作者: Catheter 時(shí)間: 2025-3-31 08:42
Evaporation in Arid and Semi-Arid Regionssed..It is pointed out that most models for evaporation are developed for temperate crops. The main differences between temperate and (semi-)arid regions are described..Special attention will be paid to the use of remote sensing techniques, for the determination of evaporation.作者: LAST 時(shí)間: 2025-3-31 11:59
