ファイル情報(添付) | |
タイトル |
砂丘地土壌の水分の保留を高める一方法について
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タイトル |
A metbod to raise the preservation of surface soil moisture on sand-dune soil
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タイトル 読み |
サキュウチ ドジョウ ノ スイブン ノ ホリュウ オ タカメル イチ ホウホウ ニツイテ
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著者 |
十川 博
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収録物名 |
島根農科大学研究報告
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巻 | 7 |
開始ページ | (A)101 |
終了ページ | 105 |
収録物識別子 |
ISSN 05598311
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内容記述 |
その他
To be improved the water economy of sand-dune soil, it was investigated to determine the effect to the preservation of surface soil moisture by laying out in the subsoil thin layer of various substances -four sois of different texture, gravel and finely cutted straw.
(1 Water was added on the column of sand-dune soil in the glass tube, and per iodical changes of soil moisture in each strata were measured. When the thin layer is consist of gravel or finely cutted straw that possess the large pore, the greater part of capillary water were reserved in the sand stratun on the thin layer for along time. Capillar rise was stagnated at the aboven-mentioned layers. 2) Generally speaking, when wet sandy soil come in contact with dry clayey soil, capillary water moved largely from the former to the latter. In opposition, when wet cleyey soil come in contact with dry sandy soil, capillary water moved slightly from the former to the latter. It rmay be reasonable that capillasy water is apt to be discontinous in the sandy soil relatively. 3) The movement of gravitational waler is affected by the perrmeability of the stratum that show most slowly percolation. In the sand-dune soil, The more clayey soil texture of thin layer is, the more peameability of total soil layer decrease severely. |
言語 |
日本語
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資源タイプ | 紀要論文 |
出版者 |
島根農科大学
The Shimane Agricultural College
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発行日 | 1959-03-31 |
アクセス権 | オープンアクセス |
関連情報 |
[NCID] AN00108241
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備考 | A,Bを含む |