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作 者:张卓 曹广超[1,2] 张富玲[1,2] 杨荣荣 陈治荣 童珊 ZHANG Zhuo;CAO Guangchao;ZHANG Fuling;YANG Rongrong;CHEN Zhirong;TONG Shan(MOE Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation, Qinghai Normal University, Xining 810008, China;Key Laboratory of Qinghai Province Physical Geography and Environmental Process, Qinghai Normal University, Xining 810008, China;Environmental Monitoring Station of Kezilsu Prefecture, Atushi 845350, Xinjiang, China)
机构地区:[1]青海师范大学,青藏高原地表过程与生态保育教育部重点实验室,西宁810008 [2]青海师范大学,青海省自然地理与环境过程重点实验室,西宁810008 [3]新疆克州环境监测站,新疆阿图什845350
出 处:《地质找矿论丛》2020年第2期246-252,共7页Contributions to Geology and Mineral Resources Research
基 金:国家重点研发计划项目(编号:2017YFC0404304);国家自然科学基金项目(编号:41361005)联合资助。
摘 要:文章以青海湖北部刚察县高寒草地为研究对象,分析测试土壤样品的各粒级组分进而计算出各粒度参数值,尝试探索土壤层剖面的土壤粒度与土壤磁化率的变化特征及其相关性。结果表明:该高寒草地土壤剖面粒度组成以粉砂为主,黏粒次之,再次是砂粒,土壤属性属于粉砂壤土—粉砂土;土壤质量磁化率总体较低,土壤物源既有基岩风化而成,又有远程物质的搬运沉积;土壤剖面上表现出两个较为明显的质量磁化率由高到低的周期演化,说明成土成壤过程经历了两个时期。土层在30 cm以上,质量磁化率与频率磁化率呈现出相反的变化趋势;30 cm以下随着越接近母岩方向,质量磁化率值呈现减小的态势。且在剖面上表现出两个较为明显的以高质量磁化率值开始、低质量磁化率结束为特征的周期演化。This paper deals with alpine grassland in the north Qinghai Lake area trying to find out relationship between soil particle size and magnetic susceptibilityby means of meassuring each soil particle size groups and calculating the particle size parameter.The results show that the the alpine grassland section was dominated by silt,then clay,sand.The soil belongs to silt loam-silt soil including the weathered materials of bed rock and the deposited long-distance-transported materials.The mass magnetic susceptibility is generally low.The soil section includes two distinct evelution cycles of mass magnetic susceptibility from high to low indicating that the soil is formed in two periods.Above 30cm of the soil layer the mass magnetic susceptibility and the frequency susceptibility change in opposite tendency;below 30cm,close to the bedrock,the mass susceptibility decrease.
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