標(biāo)題: Titlebook: ; [打印本頁(yè)] 作者: 注射 時(shí)間: 2025-3-21 17:14
書(shū)目名稱(chēng)Groundwater Dynamics in Hard Rock Aquifers影響因子(影響力)
書(shū)目名稱(chēng)Groundwater Dynamics in Hard Rock Aquifers影響因子(影響力)學(xué)科排名
書(shū)目名稱(chēng)Groundwater Dynamics in Hard Rock Aquifers網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱(chēng)Groundwater Dynamics in Hard Rock Aquifers網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱(chēng)Groundwater Dynamics in Hard Rock Aquifers被引頻次
書(shū)目名稱(chēng)Groundwater Dynamics in Hard Rock Aquifers被引頻次學(xué)科排名
書(shū)目名稱(chēng)Groundwater Dynamics in Hard Rock Aquifers年度引用
書(shū)目名稱(chēng)Groundwater Dynamics in Hard Rock Aquifers年度引用學(xué)科排名
書(shū)目名稱(chēng)Groundwater Dynamics in Hard Rock Aquifers讀者反饋
書(shū)目名稱(chēng)Groundwater Dynamics in Hard Rock Aquifers讀者反饋學(xué)科排名
作者: NIP 時(shí)間: 2025-3-21 20:32 作者: 600 時(shí)間: 2025-3-22 01:39 作者: 吝嗇性 時(shí)間: 2025-3-22 07:16 作者: nutrients 時(shí)間: 2025-3-22 10:22 作者: SLAY 時(shí)間: 2025-3-22 15:38 作者: SLAY 時(shí)間: 2025-3-22 19:18 作者: 口音在加重 時(shí)間: 2025-3-22 21:58
Working at the Edge of Extinction, measurements are made at two different locations, the closer the measurement points are to each other, the closer the measured values. These variables are given the name of Regionalized Variables (Re. V).作者: 誘使 時(shí)間: 2025-3-23 02:16
https://doi.org/10.1007/978-3-031-39221-4d to fill the data gap, at the time when the water level could not be measured. With this we obtained a mixed time series of water level at any well containing measured water levels without any error term and the estimated water level with estimation errors at uniform frequency.作者: 虛情假意 時(shí)間: 2025-3-23 06:34
Hydrogeological Research in India in Managing Water Resources, (690 km. from surface water and 450 km. from groundwater). The present utilization is 750 km. (500 km. from surface water and 250 km. from groundwater). The projected demand for the year 2025 is 1050 km. indicating that by that point of time the total available water resources have to be put to use.作者: vertebrate 時(shí)間: 2025-3-23 11:43 作者: Presbycusis 時(shí)間: 2025-3-23 16:11 作者: dapper 時(shí)間: 2025-3-23 18:29 作者: Ostrich 時(shí)間: 2025-3-24 01:14
Nature of Hard Rock Aquifers: Hydrogeological Uncertainties and Ambiguities,ying extent. Usually, crystalline (igneous and metamorphic) rocks are included in this group. As the hydraulic properties of these rocks are mainly controlled by fracturing, these are also referred as fractured rocks. Unlike sedimentary rocks, the hard rocks generally represent anisotropic and heterogeneous media.作者: Obituary 時(shí)間: 2025-3-24 05:31
Writing is More Than Draft and Good CopyThus the benefits to be accrued from an additional measurement could be studied prior to its measurement. Monitoring through an optimal network can reduce the amount of data required while providing the desired accuracy and a few simple procedures have been developed for a geostatistical optimization of the monitoring network in this study.作者: 爭(zhēng)論 時(shí)間: 2025-3-24 07:37
Kriging for Estimating Hydrogeological Parameters,Thus the benefits to be accrued from an additional measurement could be studied prior to its measurement. Monitoring through an optimal network can reduce the amount of data required while providing the desired accuracy and a few simple procedures have been developed for a geostatistical optimization of the monitoring network in this study.作者: crescendo 時(shí)間: 2025-3-24 13:24
James Bradbeer,Abdul Ghafoor Abdul RaheemThe most important aspect of groundwater studies in an area is to determine how much groundwater can be safely withdrawn and also for management of the available source. This determination involves作者: Mercurial 時(shí)間: 2025-3-24 18:11 作者: 有權(quán)威 時(shí)間: 2025-3-24 20:22 作者: ADORN 時(shí)間: 2025-3-25 02:15 作者: Coronation 時(shí)間: 2025-3-25 05:57
Application of Remote Sensing and GIS in Groundwater Exploration,emarcate the groundwater potential zones. Therefore, an integrated approach, including studies of lithology, hydrogeomorphology and lineament, has been taken up, using remote sensing and GIS techniques, for a proper assessment of groundwater potential zones in the study area.作者: 四牛在彎曲 時(shí)間: 2025-3-25 10:19
Various Pumping Tests and Methods for Evaluation of Hydraulic Properties in Fractured Hard Rock Aquues, and that they vary from negligible up to a factor of about three for higher . values. (.), from hydrological tests on dug wells in the crystalline rocks, estimated a range of . values from 26.5 to 56.36 m./d, for the weathered zone based on interpretation made by Papodopulos and Cooper method (作者: 名詞 時(shí)間: 2025-3-25 15:41
Analyses of Aquifer Parameters from Different Hydraulic Tests and Their Scale Effect,or suppression which can be related to a pumping or injection tests. The corresponding changes in water levels are recorded in the bore-well with the help of a water level recorder. With this record of the rate of recovery or recession of the water level, the transmissivity or the hydraulic conducti作者: 嗎啡 時(shí)間: 2025-3-25 19:25
Upscaling of Slug Test Hydraulic Conductivity Using Discrete Fracture Network Modelling in Graniticoited on a large scale. But this uncontrolled exploitation of the resource has resulted in an alarming decline in water levels. The characterization of the flow and storage of ground water in these systems is a challenging task since flow and transport processes are very different from those occurri作者: 強(qiáng)所 時(shí)間: 2025-3-25 20:11
Water Budgeting and Construction of Future Scenarios for Prediction and Management of Ground Water s have been prepared. It is observed that both water balances for a “bad” and “good” monsoon could more or less be counterbalanced, the water balance is negative for a normal monsoon inducing a depletion of the Water Table at about 1 m/year due to consecutive deficit rainfall years. Due to this, in 作者: 本土 時(shí)間: 2025-3-26 00:41 作者: 處理 時(shí)間: 2025-3-26 05:08
Simulation of Flow in Weathered-Fractured Aquifer in a Semi-Arid and Over-Exploited Region, of overexploitation of its weathered hard rock aquifer, its cropping pattern, rural socio-economy, agricultural practices and semi-arid climate. The objective of this study is to develop and test well-suited modelling approaches to simulate the flow in the existing aquifer system that consist of tw作者: 帶來(lái)的感覺(jué) 時(shí)間: 2025-3-26 11:25 作者: AXIOM 時(shí)間: 2025-3-26 14:47 作者: ornithology 時(shí)間: 2025-3-26 18:17
emarcate the groundwater potential zones. Therefore, an integrated approach, including studies of lithology, hydrogeomorphology and lineament, has been taken up, using remote sensing and GIS techniques, for a proper assessment of groundwater potential zones in the study area.作者: 半球 時(shí)間: 2025-3-26 21:12
https://doi.org/10.1007/978-981-4021-84-5ues, and that they vary from negligible up to a factor of about three for higher . values. (.), from hydrological tests on dug wells in the crystalline rocks, estimated a range of . values from 26.5 to 56.36 m./d, for the weathered zone based on interpretation made by Papodopulos and Cooper method (作者: 谷類(lèi) 時(shí)間: 2025-3-27 03:28 作者: DENT 時(shí)間: 2025-3-27 06:32 作者: Nonporous 時(shí)間: 2025-3-27 11:52
Pedagogy and Psychology in Digital Educations have been prepared. It is observed that both water balances for a “bad” and “good” monsoon could more or less be counterbalanced, the water balance is negative for a normal monsoon inducing a depletion of the Water Table at about 1 m/year due to consecutive deficit rainfall years. Due to this, in 作者: Sleep-Paralysis 時(shí)間: 2025-3-27 15:58 作者: 連詞 時(shí)間: 2025-3-27 20:50 作者: laxative 時(shí)間: 2025-3-27 23:34 作者: 不吉祥的女人 時(shí)間: 2025-3-28 03:14
Pedestrian Fall Safety Assessmentso some degree with a scale ranging from microcracks to crustal rifts (.). The fractures generally increase the hydraulic conductivity of the rocks if the discontinuities are more permeable than the parent rock. Sometimes fractures may form barriers to flow if the contained material is less permeable作者: CAJ 時(shí)間: 2025-3-28 09:24 作者: 依法逮捕 時(shí)間: 2025-3-28 10:48
Nature of Hard Rock Aquifers: Hydrogeological Uncertainties and Ambiguities,nt primary (intergranular) porosity and primary permeability. However, weathering and fracturing can impart secondary porosity and permeability to varying extent. Usually, crystalline (igneous and metamorphic) rocks are included in this group. As the hydraulic properties of these rocks are mainly co作者: eulogize 時(shí)間: 2025-3-28 18:09
Overview of the Hydrogeology of Hard Rock Aquifers: Applications for their Survey, Management, Modepe, etc.). Their groundwater resources are modest in terms of available discharge per well (from less than 2-3 m./h up to 20 m./h), compared to those in other types of aquifers (sedimentary, karstic or volcanic aquifers). They are, however, geographically widespread and therefore well suited to scat作者: 欺騙手段 時(shí)間: 2025-3-28 22:01 作者: Tidious 時(shí)間: 2025-3-29 00:01 作者: 羊齒 時(shí)間: 2025-3-29 05:39 作者: abracadabra 時(shí)間: 2025-3-29 08:15
Analyses of Aquifer Parameters from Different Hydraulic Tests and Their Scale Effect,uddenly added or removed from the well. However one limitation of conducting slug tests in this manner is that if the tests are being conducted for environmental monitoring purposes it is not advisable to inject or take out a certain volume of water in the well as it may disturb the ambient water qu作者: violate 時(shí)間: 2025-3-29 13:08 作者: 簡(jiǎn)略 時(shí)間: 2025-3-29 18:26
Water Budgeting and Construction of Future Scenarios for Prediction and Management of Ground Water rock aquifers in granitic area by taking a small watershed at Maheshwaram, RR Dist of Andhra Pradesh and has developed a number of specific techniques during five years for aquifer characterization, groundwater balance both global and discretized including the technique of the “Double Water Table F作者: 可互換 時(shí)間: 2025-3-29 20:23
Applying Geostatistics: Basic Knowledge and Variographic Analysis with Exercises,of the physical system. In most cases these parameters change their values in space and sometimes in time also and hence they are called variables. Rainfall, effective recharge, thickness of an aquifer, hydraulic head, transmissivity, permeability, storage coefficient, etc. are the examples in hydro作者: 軍械庫(kù) 時(shí)間: 2025-3-30 03:38 作者: 冷淡一切 時(shí)間: 2025-3-30 06:25
Application of Geostatistics in Optimal Groundwater Monitoring Network Design,on on isolated location mainly in the field of hydrogeology makes it necessary to adopt special procedures such as geostatistical estimation technique for bridging the gap between field measurements and data requirements. However, these estimations are based on a crucial criterion of the structural 作者: 言外之意 時(shí)間: 2025-3-30 10:09 作者: figment 時(shí)間: 2025-3-30 13:22 作者: 硬化 時(shí)間: 2025-3-30 16:42 作者: 使激動(dòng) 時(shí)間: 2025-3-30 21:49
Regional Simulation of a Groundwater Flow in Coastal Aquifer, Tamil Nadu, India,. During the past two decades, the water level in several parts of India has been falling rapidly due to increase in pumping of ground waters. Proper management of aquifer systems is necessary as groundwater is the major source for domestic and industrial purposes, especially in urban and semi urban作者: MUT 時(shí)間: 2025-3-31 01:44 作者: 必死 時(shí)間: 2025-3-31 06:44
Marcello Giovanelli,Chloe Harrison groundwater situations in different parts of the country are divergent. Uneven distribution of surface water in space and time, man’s interference, and over-exploitation of groundwater have caused regional imbalances in the supply and demand of water both in the alluvial tract of north India and in作者: 牽索 時(shí)間: 2025-3-31 10:32
Maja Dekovi?,Jessica Asscher,Sabine Stoltznt primary (intergranular) porosity and primary permeability. However, weathering and fracturing can impart secondary porosity and permeability to varying extent. Usually, crystalline (igneous and metamorphic) rocks are included in this group. As the hydraulic properties of these rocks are mainly co作者: 解凍 時(shí)間: 2025-3-31 14:20 作者: conscience 時(shí)間: 2025-3-31 18:49
Robyn Brandenburg,Jacqueline Z. Wilsonnce past few years due to rapid development and advancement in microprocessors and associated numerical modelling solutions. Although geophysics has ability to probe deep earth interior (say >1000 m), but its application for groundwater studies is usually restricted to depths less than and around 25作者: 寒冷 時(shí)間: 2025-4-1 01:15
ool in groundwater prospecting (.; .; .; .; .). The remote sensing data helps in fairly accurate hydrogeomorphological analysis and identification and delineation of land features (.). With sufficient ground data, hydrological characteristics of geomorphological features can be deciphered. Groundwat
