Morphological Feature and Physicochemical Characteristics of Soils under Festuca spp. Dominant Steppe at High Mountain and Mountain of Khuvsgul, Mongolia  

作　　者：Saruul Narangerel Undarmaa Jamsran Maki Asano Kenji Tamura Saruul Narangerel;Undarmaa Jamsran;Maki Asano;Kenji Tamura(School of Life and Environmental Sciences, University of Tsukuba, Ibaraki, Japan;Center for Ecosystem Studies, Mongolian University of Life Sciences, Ulaanbaatar, Mongolia;Faculty of Life and Environmental Sciences, University of Tsukuba, Ibaraki, Japan)

机构地区：[1]School of Life and Environmental Sciences, University of Tsukuba, Ibaraki, Japan [2]Center for Ecosystem Studies, Mongolian University of Life Sciences, Ulaanbaatar, Mongolia [3]Faculty of Life and Environmental Sciences, University of Tsukuba, Ibaraki, Japan

出　　处：《Open Journal of Soil Science》2022年第9期446-474,共29页土壤科学期刊（英文）

摘　　要：The morphology, physicochemical, humic substances and micromorphological characteristics of four soil profiles of the steppe dominant by Festuca lenensis (F. lenensis) at the high mountain and mountain of Khuvsgul, Mongolia were studied. Soils were classified as Regosols and Leptosols at high mountain steppe, Leptosols and Cambisols at mountain steppe. On a high mountain, the plant root distribution, OC, N and moisture contents were high due to its high precipitation and low temperature. The soils show immature characteristics with low available nutrients, weakly developed crumb structure, many semi- and undecomposed plant residues, and few little organic pigments with few excrements. The humic acids with immature to degraded characteristics indicate that the climatic condition of high mountains inhibits the soil decomposition process. Due to extremely different landform positions, there a sharp difference was observed between studied soils on high mountain steppe. On the summit with a flat position, the soil of TSO1 showed finer soil texture with higher CEC, exchangeable Mg²⁺ and humification degree of SOM compared with the soil of TSO2, which located on the steep slope. This confirms that the abrupt changes in landform on high mountain strongly affect the properties of topsoil. On the mountain steppe, the soil contains higher exchangeable Na⁺, exchangeable K⁺ and water soluble at topsoil;however, the plant root distribution, OC, N and moisture contents were lower than that of high mountain soil. Because of warmer air and soil temperature in comparison with that of high elevation, active turnover in humic horizon and chemical weathering process lead to higher available nutrients in mountain steppe. The degraded to well humified characteristics of humic acid, moderately developed crumb structure, a higher component of little organic pigment and many intact excrements indicate that the soil decomposition process and biological activity were higher than that of the high mountain steThe morphology, physicochemical, humic substances and micromorphological characteristics of four soil profiles of the steppe dominant by Festuca lenensis (F. lenensis) at the high mountain and mountain of Khuvsgul, Mongolia were studied. Soils were classified as Regosols and Leptosols at high mountain steppe, Leptosols and Cambisols at mountain steppe. On a high mountain, the plant root distribution, OC, N and moisture contents were high due to its high precipitation and low temperature. The soils show immature characteristics with low available nutrients, weakly developed crumb structure, many semi- and undecomposed plant residues, and few little organic pigments with few excrements. The humic acids with immature to degraded characteristics indicate that the climatic condition of high mountains inhibits the soil decomposition process. Due to extremely different landform positions, there a sharp difference was observed between studied soils on high mountain steppe. On the summit with a flat position, the soil of TSO1 showed finer soil texture with higher CEC, exchangeable Mg²⁺ and humification degree of SOM compared with the soil of TSO2, which located on the steep slope. This confirms that the abrupt changes in landform on high mountain strongly affect the properties of topsoil. On the mountain steppe, the soil contains higher exchangeable Na⁺, exchangeable K⁺ and water soluble at topsoil;however, the plant root distribution, OC, N and moisture contents were lower than that of high mountain soil. Because of warmer air and soil temperature in comparison with that of high elevation, active turnover in humic horizon and chemical weathering process lead to higher available nutrients in mountain steppe. The degraded to well humified characteristics of humic acid, moderately developed crumb structure, a higher component of little organic pigment and many intact excrements indicate that the soil decomposition process and biological activity were higher than that of the high mountain ste

关 键 词：Soil Micromorphology Soil Physicochemical Festuca lenensis Mountain Steppe Khuvsgul 

分 类 号：S15[农业科学—土壤学]