长江源多年冻土区热融湖塘的形成对土壤沙化过程的影响

高泽永; 王一博; 文晶; 盛兆海

doi:10.7522/j.issn.1000-694X.2013.00376

中国沙漠 >

2014 , Vol. 34 >Issue 3: 758 - 764

DOI: https://doi.org/10.7522/j.issn.1000-694X.2013.00376

生物与土壤

长江源多年冻土区热融湖塘的形成对土壤沙化过程的影响

高泽永 ,
王一博 ,
文晶 ,
盛兆海

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1. 兰州大学资源与环境学院, 甘肃兰州 730000;
2. 中国科学院寒区旱区环境与工程研究所冻土工程国家重点实验室, 甘肃兰州 730000;
3. 格尔木市气象局五道梁气象站, 青海格尔木 816000

高泽永（1990-），男，甘肃庆阳人，硕士研究生，主要从事寒区旱区水文过程的研究。Email：gaozy12@lzu.edu.cn

收稿日期: 2013-05-08

修回日期: 2013-07-07

网络出版日期: 2014-05-20

基金资助

国家自然科学基金项目（41271092）；冻土工程国家重点实验室开放基金项目（SKLFSE201109）资助

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The Influence of Thermokarst Lake Formation on Soil Desertification Process in Permafrost Regions of the Source Region of the Yangtze River

Gao Zeyong ,
Wang Yibo ,
Wen Jing ,
Sheng Zhaohai

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1. College of Earth and Environment Sciences, Lanzhou University, Lanzhou 730000,China;
2. State Key laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
3. Weather Station of Wudaoliang, Golmud Meteorological Bureau, Golmud 816000, Qinghai, China

Received date: 2013-05-08

Revised date: 2013-07-07

Online published: 2014-05-20

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摘要

选择长江源区五道梁为研究区域，以典型发育的热融湖塘为研究对象，运用激光粒度仪测得土壤粒径分布，并结合分形模型对高寒草甸土壤颗粒分布与水文过程进行研究。结果表明：热融湖塘的形成加快了长江源区高寒草甸土壤沙质化的进程，随着其影响程度的加剧，黏粒、粉粒含量逐渐减小，砂粒含量逐渐增大，同时土壤颗粒体积分形维数也逐渐减小，并与黏粒、粉粒呈显著正相关，与砂粒含量呈显著负相关，土壤颗粒体积分形维数可代替土壤不同粒径颗粒组成表征土壤沙质化的进程。此外，在热融湖塘影响下的土壤水文过程的改变，是加快土壤沙质化的重要因素之一。

关键词： 热融湖塘; 长江源区; 颗粒分形维数; 沙化过程

本文引用格式

高泽永 , 王一博 , 文晶 , 盛兆海 . 长江源多年冻土区热融湖塘的形成对土壤沙化过程的影响[J]. 中国沙漠, 2014 , 34(3) : 758 -764 . DOI: 10.7522/j.issn.1000-694X.2013.00376

Abstract

We chose Wudaoliang in the source region of the Yangtze River as the study area and a typically developed thermokarst lake as the study object, using the laser diffraction method to measure the soil particle size distribution (PSD), and studied the PSD and hydrological process of alpine meadow soil combined with a fractal model. The results show that the formation of the thermokarst lake speeds up the desertification of alpine meadow soil in the source region of the Yangtze River. As the affect intensifies, the share of clay particle (0-2 μm) and silt particle (2-50 μm) gradually decreases, while the share of sand particle (50-2000 μm) increases. Meanwhile, the volume fractal dimension also reduces gradually, showing a significant positive linear correlation with the share of clay particle and silt particle and a significant negative linear correlation with the share of sand particle. Volume fractal dimension of soil can substitute for PSD to characterize the process of soil desertification. In addition, soil hydrological process changes under the influence of thermokarst lakes, which is one of the important factors speeding up soil desertification.

Key words： thermokarst lake; the source region of the Yangtze River; fractal dimension of particle size distribution; desertification

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