吉林大学学报(地球科学版)

• 地质工程与环境工程 • 上一篇    下一篇

基于现场热响应测试方法的地下岩土热物性分析

刘春雷1,王贵玲1,王婉丽1,蔺文静2   

  1. 1.中国地质科学院水文地质环境地质研究所,石家庄050061;
    2.中国地质大学(北京)水资源与环境学院,北京100083
  • 收稿日期:2013-12-03 出版日期:2014-09-26 发布日期:2014-09-26
  • 通讯作者: 蔺文静(1978-),男,副研究员,博士,主要从事水文地质和地热地质研究工作 E-mail:lwenjing@msn.com
  • 作者简介:刘春雷(1985-),男,研究实习员,硕士,主要从事水文地质和地热地质研究工作,E-mail:chunleiliudn@163.com
  • 基金资助:

    国家自然科学基金项目(41302189);国家“863”计划项目(2012AA052802)

Analysis of  Soil Thermal Properties with In-Situ Thermal Response Test Method

Liu Chunlei1, Wang Guiling1, Wang Wanli1, Lin Wenjing2   

  1. 1.Institute of Hydrogeology and Environmental Geology,Chinese Academy of Geological Sciences,Shijiazhuang050061, China;
    2.School of Water Resources and Environment,China University of Geosciences,Beijing100083,China
  • Received:2013-12-03 Online:2014-09-26 Published:2014-09-26

摘要:

目前获取导热系数的主要方法是现场热响应试验,但该方法缺乏统一的技术标准,导致计算结果可比较性差,难以应用。笔者开展了不同热响应试验设备的原位热物性测试系列试验,分析了测试与数据处理方法对测试结果的影响,探讨了试验过程中需要注意的问题。结果显示:为减少试验误差,两次热响应试验测试的时间间隔不应少于10 d;应尽量避免循环水与岩土介质以外的其他介质产生热量交换;对于恒热流热响应试验,导热系数值与舍弃时间(1.0~12.0 h)成正相关关系;而对于定进回循环水温差的热响应试验,导热系数值与舍弃时间(0.0~12.0 h)成负相关关系;舍弃时间大于12.0 h时,导热系数变化趋于稳定。按统一标准舍弃前12.0 h的测试数据进行导热系数计算,6家单位的导热系数计算值都在2.2~2.8 W/(m·℃)范围内,测试结果合理可靠。

关键词: 地源热泵, 现场热响应试验, 岩土热物性

Abstract:

At present, in-situ thermal response test is widely used to measure thermal conductivity parameter in engineering. However, due to the lack of unified technical standard of the test, results obtained from in-situ test have unsatisfactory reliability. Our main aim is to analyze the effects of test methods and data processing on the results of the tests. Series of in-situ tests were carried out by using various of thermal response equipments in a special test well. Results show that in order to reduce experimental error, time interval between two thermal response tests should not be less than 10 days and circulating water should be prevented from heat exchange with other media(except for geotechnical media). For thermal response tests with steady input power, the value of thermal conductivity is positively correlated with times not used(1.0-12.0 h). On the other hand, for thermal response tests with steady temperature difference, the thermal conductivity value  is negatively correlated with times not used (0.0-12.0 h).It is also found that the value of thermal conductivity is stabilized with times not used (>12.0 h). According to the uniform standard with times not used (>12.0 h), the values of thermal conductivity of the six units are all within 2.2-2.8 W/(m·℃), and the test results are reasonable and reliable.

Key words: ground source heat pump, in-situ thermal response test, soil thermal properties

中图分类号: 

  • P314
[1] 陈宝义, 岳韬, 曹品鲁, 王如生, 王茂森, 博坤, 龙翔, 鲁思宇. 挤密条件下U型地埋管换热器换热效率的理论分析及数值模拟[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1808-1814.
[2] 张庆,张延军,周炳强,黄贤龙,于子望,孙永泉. 天然冷源对地下水源热泵的影响规律[J]. 吉林大学学报(地球科学版), 2013, 43(2): 537-543.
[3] 张楠, 孙友宏, 王庆华. 基于组态软件、智能模块及PLC的岩土热物性原位测试仪监控系统[J]. J4, 2010, 40(2): 383-388.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!