土壌の物理性
Online ISSN : 2435-2497
Print ISSN : 0387-6012
足柄平野扇状地における不飽和帯水層の水分測定
濱田 浩正二平 聡宮下 雄次
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2000 年 84 巻 p. 43-47

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Most of irrigated water in paddy fields infiltrates underground. This process, however, has not been clarified. In the case that groundwater table is deep, the measurement of water content in unsaturated aquifer has not been reported. We measured water content in unsaturated aquifer in the Ashigara Alluvial Fan using neutron moisture meter. As a result, there was no difference in the water content between in irrigation period and in non-irrigation. It was revealed that the infiltrated water from the paddy fields goes down, not increasing water content in unsaturated aquifer in the Ashigara Alluvial Fan.
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© 2000 土壌物理学会
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