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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Takir (soil) ： ウィキペディア英語版 Takir (soil) Takir (Takyr) ((ロシア語:Такыр), originally from Kazakh or another Turkic language) is a type of relief occurring in the deserts of Central Asia, similar to a salt flat in the southwestern United States. A takyr is usually formed in a shallow depressed area with a heavy clay soil, which is submerged by water after seasonal rains. After the water evaporates, a dried crust with fissures forms on the surface. The crust is primarily formed by filamentous cyanobacteria. == Further reading == * Jayne Belnap, Otto Ludwig Lange. "Biological Soil Crusts: Structure, Function, and Management". Springer, 2001, ISBN 3-540-43757-6. Page 90, Chapter 7.5, "Central Asia Takyr". 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Takir (soil)」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.