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Effect of Bypass-Flow on Leaching of Salts in a Cracking Soil in the Nile Delta

https://repository.lib.tottori-u.ac.jp/records/7394
https://repository.lib.tottori-u.ac.jp/records/7394
30828ac5-d0b0-4b02-b2c7-b29e240bf034
名前 / ファイル ライセンス アクション
wtr13(7)_w13070993.pdf wtr13(7)_w13070993.pdf (4.8 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2022-09-08
タイトル
タイトル Effect of Bypass-Flow on Leaching of Salts in a Cracking Soil in the Nile Delta
言語 en
言語
言語 eng
キーワード
主題 salinity stress
キーワード
主題 solute transport
キーワード
主題 preferential flow
キーワード
主題 drainage
キーワード
言語 en
主題 salinity stress
キーワード
言語 en
主題 solute transport
キーワード
言語 en
主題 preferential flow
キーワード
言語 en
主題 drainage
資源タイプ
資源タイプ journal article
著者 藤巻, 晴行

× 藤巻, 晴行

WEKO 4874
e-Rad 90323253
研究者総覧鳥取大学 100000694

藤巻, 晴行

ja-Kana フジマキ, ハルユキ

en Fujimaki, Haruyuki

Search repository
Abd, El Baki Hassan Mohamed Fahmy

× Abd, El Baki Hassan Mohamed Fahmy

WEKO 27505

en Abd, El Baki Hassan Mohamed Fahmy

Search repository
著者所属(英)
言語 en
値 Arid Land Research Center, Tottori University
著者所属(英)
言語 en
値 Arid Land Research Center, Tottori University
抄録
内容記述タイプ Other
内容記述 Salinity is a major threat to the sustainability of irrigated agriculture in arid and semi-arid regions. Leaching is the primary measure for removing excess salts from the root zone, but not all water applied to the soil surface contributes to the removal of salts. In clayey soils, bypass flow along cracks can occur without being mixed with saline pore water in the matrix. To present a field dataset to quantitatively evaluate the contribution of bypass flow to the leaching of salts, soil sampling and monitoring of groundwater and discharge from a tile drain were carried out in farmland having a cracking soil in the Nile Delta. The electrical conductivities of 1:2 extracts were measured to evaluate the salinity of the soil. The first evidence for the occurrence of significant bypass flow through cracks was the salinity of the pore water, which was nearly triple that of the shallow groundwater and outflow from drainage. Second, the difference in root zone salinity before and after paddy rice cultivation was not significant. Third, the gradient of the groundwater table was very small. in spite of the low saturated hydraulic conductivity. Fourth, the salinity of the outflow from the tile drain dropped just after irrigation or rain. These results indicated that bypass flow through cracks played a significant role in the drainage process in the soil, and that nearly half of the water bypasses through cracks in the field with a cracking soil.
書誌情報 WATER
en : WATER

巻 13, 号 7, p. 993, 発行日 2021-04
出版者
出版者 MDPI
DOI
関連タイプ isIdenticalTo
識別子タイプ DOI
関連識別子 10.3390/w13070993
権利
権利情報 (C) 2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
情報源
関連名称 Fujimaki Haruyuki, Abd El Baki Hassan Mohamed Fahmy. Effect of Bypass-Flow on Leaching of Salts in a Cracking Soil in the Nile Delta. WATER. 2021. 13(7). doi:10.3390/w13070993
関連サイト
識別子タイプ DOI
関連識別子 https://doi.org/10.3390/w13070993
関連名称 https://doi.org/10.3390/w13070993
著者版フラグ
出版タイプ VoR
EISSN
値 20734441
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