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基于GIS空间分析模型的祁连山多年冻土研究

傅连珍 胡道功 张绪教 游报捷 吴泽群 叶梦旎

傅连珍, 胡道功, 张绪教, 等, 2015. 基于GIS空间分析模型的祁连山多年冻土研究. 地质力学学报, 21 (3): 371-377.
引用本文: 傅连珍, 胡道功, 张绪教, 等, 2015. 基于GIS空间分析模型的祁连山多年冻土研究. 地质力学学报, 21 (3): 371-377.
FU Lian-zhen, HU Dao-gong, ZHANG Xu-jiao, et al., 2015. STUDY ON PERMAFROST OF QILIAN MOUNTAINS BASED ON GIS SPATIAL ANALYSIS MODEL. Journal of Geomechanics, 21 (3): 371-377.
Citation: FU Lian-zhen, HU Dao-gong, ZHANG Xu-jiao, et al., 2015. STUDY ON PERMAFROST OF QILIAN MOUNTAINS BASED ON GIS SPATIAL ANALYSIS MODEL. Journal of Geomechanics, 21 (3): 371-377.

基于GIS空间分析模型的祁连山多年冻土研究

基金项目: 

中国地质调查局“陆域天然气水合物分布特征及资源潜力评价(力学所)”项目( GZH201400304

详细信息
    作者简介:

    傅连珍(1990-), 女, 硕士研究生。主要从事第四纪地质和地理信息系统应用研究。E-mail:yesterdayfu@163.com

  • 中图分类号: P642.14

STUDY ON PERMAFROST OF QILIAN MOUNTAINS BASED ON GIS SPATIAL ANALYSIS MODEL

  • 摘要: 依据祁连山和青藏高原气温、地温、冻土厚度与经纬度以及海拔的经验公式, 通过ArcGIS空间分析, 获得了祁连山地区年均气温、年均地温和冻土厚度的空间分布规律。祁连山多年冻土区年均气温和年均地温分别为-12~-6 ℃和-4~-2 ℃, 多年冻土厚度变化于90~140 m之间。其中, 哈拉湖地区海拔4300 m以上的高山区温度最低、冻土最厚, 年均气温和年均地温分别低于-10 ℃和-4 ℃, 多年冻土厚度大于140 m。结合祁连山烃源岩区域分布特征和木里天然气水合物钻孔的冻土厚度资料, 认为中祁连盆-山构造地貌发育区为天然气水合物成藏最有利区域。

     

  • 图  1  祁连山地貌及冻土类型分布(冻土类型边界据文献[6])

    Figure  1.  Geomorphology and permafrost type distribution of Qilian Mountains

    图  2  冻土参数提取流程

    Figure  2.  The flow diagram of permafrost parameters extraction

    图  3  祁连山年均气温分布图(单位:℃)

    Figure  3.  Distribution of mean annual temperature in Qilian Mountains

    图  4  祁连山年均地温分布图(单位:℃)

    Figure  4.  Distribution of mean annual ground temperature in Qilian Mountains

    图  5  祁连山多年冻土厚度分布图(单位:m)

    Figure  5.  Distribution of permafrost thickness in Qilian Mountains

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出版历程
  • 收稿日期:  2015-03-25
  • 刊出日期:  2015-09-01

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