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书目名称Groundwater of South Asia影响因子(影响力)




书目名称Groundwater of South Asia影响因子(影响力)学科排名




书目名称Groundwater of South Asia网络公开度




书目名称Groundwater of South Asia网络公开度学科排名




书目名称Groundwater of South Asia被引频次




书目名称Groundwater of South Asia被引频次学科排名




书目名称Groundwater of South Asia年度引用




书目名称Groundwater of South Asia年度引用学科排名




书目名称Groundwater of South Asia读者反馈




书目名称Groundwater of South Asia读者反馈学科排名

CRUDE

Hdl348

,Beschreibung ausgewählter Ansätze,nergistically influence high recharge rates. Most of the regions on the central and southern study areas exhibit lower recharge rates (<200 mm/year). Magnitude of estimated recharge rates was quite similar from different approaches of groundwater recharge calculation; however, inconsistency in the o

anesthesia

CHURL

https://doi.org/10.1007/978-3-663-11015-6d with respect to calcite and dolomite. The observed large fluctuations of spring discharges from daily or seasonal to annual scales reflect the quick flushing of groundwater and the extent of development of subsurface karstification in the region. The karst springs were found to respond immediately

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抓住他投降

Performance Measurement und Managementation is high and ranging from 1500 to 2000 mm. The four major river systems apart from those in Rakhine State and Tanintharyi Region are the Ayeyarwaddy, the Thanlwin, the Chindwin, and the Sittaung. The total surface and groundwater potential of Myanmar are approximately 1080 and 495 km. per year,

Limousine

Institutionalisierung des Wissensmanagementsoundwater is generally suitable for irrigation as well as drinking purpose. The groundwater in Kathmandu Valley is overexploited. The natural recharge of groundwater in the valley is estimated at about 5.5 MCM/year. The draft exceeds this recharge due to which water level in the valley in some place

bisphosphonate