艾比湖地区南北典型断面的土壤粒度特征  

Characteristics of soil grain size in the southern and northern transections of Ebinur Lake region

作　　者：常轶深[1,2] 钱亦兵[1] 王忠臣[3] 马玉娥[1,2] 杨林[4] 

机构地区：[1]中国科学院新疆生态与地理研究所,新疆乌鲁木齐830011 [2]中国科学院研究生院,北京100049 [3]环保部环境发展中心,北京100029 [4]塔里木油田公司矿区服务事业部,新疆库尔勒841000

出　　处：《干旱区地理》2012年第6期968-977,共10页Arid Land Geography

基　　金：国家重点基础研究发展计划资助项目(2009CB825105);国家自然科学基金面上项目(41171157)

摘　　要：通过对艾比湖典型断面土壤粒度特征分析,发现研究区粒径组成以中粉沙为主,质地以砂质壤土为主,土壤垂向粗骨化明显。土壤分选性较差,粒度分布多为正偏,峰态多为窄峰态,表明该区土壤母质来源丰富,搬运一沉积环境异质性显著,但流水作用突出。北断面的分维值高于南断面,这与南断面分选性好于北断面相吻合。不同地区的概率累计曲线类型各异,但都富含悬移组分,并且对环境敏感的粒度组分大都在60μm上下,说明研究区土壤母质以水成沉积环境为主的基础上,叠加有风成碎屑。In August 2010, the field investigation was conducted in the southern and northern transections of the Ebinur Lake region, and different vegetation parameters and 39 soil samples were collected according to the natural conditions of geomorphology, vegetation, and soil in this study. The elevation was obtained with GPS positioning for each sample site. The physical-chemical properties of 78 soil samples, which were collected according to the layers of soil genesis, were analyzed in the lab. The composition of grain-sizes of soil samples was measured using Malv- ern - 2 000 for the range of O. 02 - 1 000 ~m and the grain-sizes of larger than 1 000 ~m were measured by me- chanical screening method. Grain-size parameters were calculated by Folk and Ward formula. The Visher cumula- tive probability size-frequency curves and environment sensitive grain-size curves also were plotted.＂ Finally, thetion-deposition for ground-surface materials, and the fluviation is marked. The fractal dimension values of soils in the northern transection are higher than that of southern transection, which indicates that the grain-sizes of sediment materials in the northern transection of the Ebinur Lake region is more fine than that in the northern transection and the sorting of soils in the northern transection is poor than that in the southern transection. The result shows that the source of materials and transport dynamics in the northern transection are more complex. The types of cumulative curves for soil grain-sizes in both northern and southern transections are varying with different landforms, which re- flects the different deposit and transport environments. Most of sensitive grain-size components to environments is a- bout 60 μm in the southern transection, showing that soil parent materials of the study area have some eolian sandy materials, and wind accumulation and erosion are coexist.

关 键 词：艾比湖 断面 粒度特征 环境 

分 类 号：P512.2[天文地球—地质学]