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Some problems relating to groundwater balance

 

作者: ISAMU KAYANE,  

 

期刊: Hydrological Sciences Journal  (Taylor Available online 1983)
卷期: Volume 28, issue 1  

页码: 125-137

 

ISSN:0262-6667

 

年代: 1983

 

DOI:10.1080/02626668309491147

 

出版商: Taylor & Francis Group

 

数据来源: Taylor

 

摘要:

The groundwater balance for the city of Nagaoka, Japan is presented as a case study. At Nakaoka there are three interesting features: (a) in winter groundwater is ejected from pipes under the roads to melt freshly fallen snow, (b) the river is hydraulically in contact with the aquifers, (c) the water table has remained quasi-stationary for the last five years despite the vast pumping programme. The main sources of recharge are: the River Shinano, deep percolation from irrigated fields, snowmelt in spring, and rainfall throughout the year. The water table was monitored using observation data from about 200 wells; during the irrigation period in August there was an inflow of groundwater, but groundwater resources were depleted in winter and spring by pumping for the snow-melting scheme. The evaluation and estimation of the components of the groundwater balance are discussed; in particular methods of measuring deep percolation either directly or indirectly are examined.

 

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