论文

乌鲁木齐河流冰椎及其利用研究

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  • 中国科学院兰州冰川冻土研究所, 兰州730000

收稿日期: 1995-04-02

  修回日期: 1996-05-02

  网络出版日期: 1996-07-20

ICE CONE AND ITS POSSIBILITY OF UTILIZATION IN THE URUMQI RIVER BASIN

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  • Lanzhou. Institute of Glaciology and Geocryology, Academia Sinica, Lanzhou 730000

Received date: 1995-04-02

  Revised date: 1996-05-02

  Online published: 1996-07-20

摘要

通过对河冰椎多年系统观测,对比分析其形成和发育,大致经过冰椎形成、发育、稳定、融化-冻结和消亡5个阶段.冰椎与稳定负温期的积温∑—t℃、土石冻(融)、空气相对湿度及水源补给形式有较高的相关性,为人工调蓄利用冰椎提供了科学依据.

本文引用格式

张志忠, 刘宗香 . 乌鲁木齐河流冰椎及其利用研究[J]. 地理科学, 1996 , 16(4) : 359 -364 . DOI: 10.13249/j.cnki.sgs.1996.04.359

Abstract

Multi-year observation on the ice cone in the Urmqi River basin indicates that the ice cone usually undergoes five stages; formation, growth, steadiness, melting-freezing and decay. It is found that the ice cone is closely correlated with the steady negative accumulated temperature, seasonal ground freezing process, relative humidity of air and water source type. The result may be useful for artificial regulation and utilization of the ice cone in the basin.

参考文献

1 Горбунов А Л., Ермолии Е Д. Наледив галив горах СрелиеЯ Азийи Казахстапа. Магернал гляииологическнх нсследованни, 1981,(41),175-180. 2 王文浚,试论乌每木齐河流域地表水与地下水的相互关系.见: 天山乌普木齐河冰川与水文研究论文集.北京: 科学出版社,1965. 109-118. 3 张志忠.乌鲁木齐河流域河冰荃本特征及其对春季径流的补给作用.见: 乌鲁木齐地区水资源若干间题研究(Ⅱ),乌鲁木齐河山这水资源形成和估算.北京,科学出版社,1992. 116-129. 4 新班减灾四十年编委会.新班减灾四十年.北京: 地展出版社,1993. 23-60. 5 白重瑗,等.山区河谷冰椎的生成及利用.中国科学院兰州冰川冻土研究所集刊,1984,(5),172-]85.
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