globalchange  > 气候变化与战略
CSCD记录号: CSCD:5634741
论文题名:
土壤冻融过程中的多层水热耦合模拟研究
其他题名: Study on Simulation of Water and Heat Transfer in Soil Freezing and Thawing
作者: 李佳1; 周祖昊2; 王浩2; 王康3
刊名: 水文
ISSN: 1000-0852
出版年: 2016
卷: 36, 期:1, 页码:258-263
语种: 中文
中文关键词: 土壤冻融 ; 水热耦合 ; 多层模型
英文关键词: WEP-L ; soil freezing and thawing ; coupled water and heat transfer ; multi-layer model ; WEP-L
WOS学科分类: GEOSCIENCES MULTIDISCIPLINARY
WOS研究方向: Geology
中文摘要: 为准确模拟土壤冻融过程中温湿度变化以及水热传递规律,以支撑寒区水循环及其对气候变化的响应研究,在国内具有自主知识产权的WEP-L模型基础上,通过添加土壤层水热耦合计算模块,细化土壤分层结构,构建了多层水热耦合模型。根据吉林省前郭灌区土壤冻融原位实验,确定了模型中的土壤水热参数,并用2011~2012年完整冻融周期内实测的土壤温度和含水率数据进行了模型验证。结果表明,模型能较好的模拟不同深度土层的温湿度变化规律,其中土壤温度模拟的平均NASH效率系数为0.752,土壤含水率和土壤冻结深度的模拟结果和实测值的变化规律较一致。
英文摘要: This work is to accurately simulate the moisture and temperature of freezing-thawing soil, which makes benefit to the research of water cycle and its response to climate change in cold regions. A novel multi-layer model that combines water and heat transfer based on the model of Water and Energy Transfer Process, WEP-L, was developed. The model predictions matched the experimental measurements in irrigation area of Qianguo well. The results shows that the new model could simulate soil temperature, soil moisture content percentage and soil freezing-thawing process in different depth. Overall, the new model can be used to simulate the distribution and transfer of soil water and heat fluxes.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/151563
Appears in Collections:气候变化与战略

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作者单位: 1.东华大学环境科学与工程学院, 流域水循环模拟与调控国家重点实验室
2.水利部水资源与水生态工程技术研究中心, 上海 210620, 中国
3.中国水利水电科学研究院, 流域水循环模拟与调控国家重点实验室
4.水利部水资源与水生态工程技术研究中心, 北京 100038, 中国
5.中国水利水电科学研究院, 流域水循环模拟与调控国家重点实验室
6.水资源与水电工程科学国家重点实验室, 北京 100038, 中国

Recommended Citation:
李佳,周祖昊,王浩,等. 土壤冻融过程中的多层水热耦合模拟研究[J]. 水文,2016-01-01,36(1):258-263
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