土壤热导率的研究现状及其进展

doi:10.7522/j.issn.1000-0240.2015.0119

冰川冻土 ›› 2015, Vol. 37 ›› Issue (4): 1067-1074.doi: 10.7522/j.issn.1000-0240.2015.0119

土壤热导率的研究现状及其进展

杜宜臻^{1 2}, 李韧¹, 吴通华¹, 谢昌卫¹, 肖瑶¹, 胡国杰¹, 王田野^{1 2}

1. 中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室青藏高原冰冻圈观测研究站, 甘肃兰州 730000;
2. 中国科学院大学, 北京 100049

收稿日期:2015-03-12 修回日期:2015-04-23 出版日期:2015-08-25 发布日期:2016-01-18
通讯作者: 李韧, E-mail: liren@lzb.ac.cn. E-mail:liren@lzb.ac.cn
作者简介:杜宜臻(1992-), 女, 山东临沂人, 2013年于曲阜师范大学获学士学位, 现为中国科学院寒区旱区环境与工程研究所在读硕士研究生, 主要从事青藏高原土壤热力特征方面的研究. E-mail: yzhdu@lzb.ac.cn
基金资助:
国家重大科学研究计划项目(2013CBA01803); 国家自然科学基金项目(41271081; 41271086; 41401085); 国家自然科学基金创新研究群体科学基金项目(41121001); 中国科学院重点部署项目(KJZD-EW-G03-02); 中国科学院百人计划项目(51Y551831001)资助

Study of soil thermal conductivity: research status and advances

DU Yizhen^{1 2}, LI Ren¹, WU Tonghua¹, XIE Changwei¹, XIAO Yao¹, HU Guojie¹, WANG Tianye^{1 2}

1. Cryosphere Research Station on the Qinghai-Tibet Plateau, State Key Laboratory of Cryosphere Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China

Received:2015-03-12 Revised:2015-04-23 Online:2015-08-25 Published:2016-01-18

摘要/Abstract

摘要： 土壤热导率是重要的土壤热参数之一, 在下垫面土壤热量的传输中起到重要作用; 同时也是区域气候模式、陆面过程模式中重要的输入参数, 在预估未来气候变化等方面也具有重要作用. 根据国内外的研究现状, 评述了土壤热导率的影响因素和模拟方案. 其中, 土壤质地、温度、含水(冰)量和孔隙度等是影响土壤热导率的主要因素, 特别在研究冻土时需重点分析含冰量的变化. 结合影响因素, 比较分析了典型的国内外计算土壤热导率的模型, 得出这些模型多适用于模拟常温下的热导率, 低温条件如青藏高原冻土区模拟结果并不理想. 因此, 多年冻土区土壤热导率的研究多基于观测资料计算或使用陆面模式中的参数化方案估算, 但因多年冻土内部水热传输过程的复杂性, 青藏高原多年冻土区热导率的模型模拟仍需进一步研究.

关键词: 土壤热导率, 影响因子, 模型, 青藏高原

Abstract: Soil thermal conductivity plays an important role in the transmission of surface soil heat into underlying soil, and also is a key parameter in the regional climate model or land surface model. In this paper, an overview of advances on soil thermal conductivity is tried to provide, and its impact factors and schemes are introduced. The thermal conductivity is significantly affected by soil texture, temperature, moisture and soil porosity, and what's more, the research of frozen soil needs to focus on the change of ice content. Then the parametric processes and the advantages and disadvantages of various models are also analyzed. However, these schemes are mostly used in simulating thermal conductivity under normal temperature, which are difficult to be applied in research of frozen soils in the Tibetan Plateau. For researching the frozen soils in the plateau, observation data or parameterized scheme of the land surface model is necessary. Due to the impact of soil freezing and thawing cycles, the thermal conductivity in the plateau still needs to be further studied.

Key words: soil thermal conductivity, impact factor, model, Tibetan Plateau

中图分类号:

S152.9

杜宜臻, 李韧, 吴通华, 谢昌卫, 肖瑶, 胡国杰, 王田野. 土壤热导率的研究现状及其进展[J]. 冰川冻土, 2015, 37(4): 1067-1074.

DU Yizhen, LI Ren, WU Tonghua, XIE Changwei, XIAO Yao, HU Guojie, WANG Tianye. Study of soil thermal conductivity: research status and advances[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2015, 37(4): 1067-1074.

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土壤热导率的研究现状及其进展

Study of soil thermal conductivity: research status and advances

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