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書目名稱Groundwater of South Asia影響因子(影響力)




書目名稱Groundwater of South Asia影響因子(影響力)學科排名




書目名稱Groundwater of South Asia網(wǎng)絡公開度




書目名稱Groundwater of South Asia網(wǎng)絡公開度學科排名




書目名稱Groundwater of South Asia被引頻次




書目名稱Groundwater of South Asia被引頻次學科排名




書目名稱Groundwater of South Asia年度引用




書目名稱Groundwater of South Asia年度引用學科排名




書目名稱Groundwater of South Asia讀者反饋




書目名稱Groundwater of South Asia讀者反饋學科排名

CRUDE

Hdl348

,Beschreibung ausgew?hlter Ans?tze,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

forager

forager

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