土壌とは? わかりやすく解説

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ど‐じょう〔‐ジヤウ〕【土壌】

読み方:どじょう

地殻最上部にある、岩石風化物に動植物遺体あるいはその分解物加わったもの。地表からの深させいぜい1、2メートルまで。つち。

作物生育させる土。「—改良

ものを発生発展させる基盤。「優秀な学者輩出する—がある」


土壌 (どじょう)

 地殻の最表層動植物とその遺体、土壌物質土質工学いうところの「土」)から気候および地形などの要因総合的な作用として歴史的に形成され自然体を指す。一定の地理的広がり持ち緑色植物生育させる能力、すなわち肥沃度を持つ点で、土壌はその母材となる岩石地層本質的に異なる。

土壌

出典: フリー百科事典『ウィキペディア(Wikipedia)』 (2023/12/27 17:28 UTC 版)

土壌(どじょう)とは、地球上の陸地の表面を覆っている鉱物有機物気体液体生物混合物である。一般には(つち)とも呼ばれる[1]。陸地および水深2.5メートル以下の水中の堆積物を指す[2]


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土壌

出典:『Wiktionary』 (2021/07/31 13:30 UTC 版)

名詞

どじょう

  1. 地質農産物育成観点から評価する語。地殼表面岩石崩壊ないし分解した無機物主成分とし、多少生物腐敗分解して生じた有機分が混合したもの。つち。つちくれ
  2. 比喩)ある文化等の現象成立する背景となっている諸要素

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