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논문 기본 정보

자료유형
학술저널
저자정보
Mijin Seo (National Academy of Agricultural Science) Kyunghwa Han (National Academy of Agricultural Science) Kangho Jung (National Academy of Agricultural Science) Heerae Cho (National Academy of Agricultural Science) Yongseon Zhang (National Academy of Agricultural Science) Seyeong Choi (Gyeongsangbuk-do Agricultural Research & Extension Services)
저널정보
한국토양비료학회 한국토양비료학회지 한국토양비료학회지 제49권 제4호
발행연도
2016.8
수록면
300 - 309 (10page)

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초록· 키워드

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The monolithic weighing lysimeter is a useful facility that could directly measure water movement via layers, drainage, and evapotranspiration (ET) with precise sensors. We evaluated water movement through layers and water balance using the lysimeter with undisturbed paddy sandy loam soil, Gangseo soil series (mesic family of Anthraquic Eutrudepts classified by Soil Taxonomy) during winter season from Dec. 2014 to Feb. 2015. Daily ET indicated up to 1.5 mm in December and January and 2 mm in February. The abrupt increase of soil water tension at the depth of 0.1 m, when soil temperature at the same depth was below 2°C, was observed due to temporary frost heaving. The surface evaporation was less than reference ET below -15 kPa of soil water potential at the depth of 0.1 m. The maximum drainage rate was similar to the saturated hydraulic conductivity of a plow pan layer. Both upward and downward water movement, related to ET and drainage, were retarded by a plow pan layer. This study demonstrated that the lysimeter study could well quantify water balance components even under frost heaving during winter season and that a plow pan with low permeability could act as a boundary that affects drainage and evapotranspiration.

목차

Introduction
Methods and Materials
Results
Discussion
Conclusions
References

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UCI(KEPA) : I410-ECN-0101-2017-523-001137130