高原山地土壤冻融对径流形成的影响研究进展
Progresses in Soil Freezing-Thawing Effects on the Runoff Generation in Plateau-Mountain Regions
查看参考文献80篇
文摘
|
亚洲主要江河的水源补给受到山地高原寒冻环境的影响,高寒山区积雪和冻土影响了江河源头的径流形成条件,是高寒环境下的具有固液两相变化的径流形成机制,在全球气候变化的大背景下对亚洲主要河流的径流变化和水资源供给具有重要作用。其中冻土的分布、发展和消融是决定该区域径流形成的一个关键环节,研究和揭示土壤冻融对径流形成的影响机制,成为研究全球气候变化和水资源安全领域的热点。要认识亚洲主要江河源头径流变化规律,预测气候变化条件下西部主要河流水资源动态,需要攻克高山(高原)地表环境要素对冻土格局的影响机制,高寒山区土壤冻融和地下水分的转化条件与阈值,冻土产汇流模型及相关参数确定方法,相关冰雪冻融—径流形成关系等关键环节。通过高寒地区冻土水文观测、土壤冻融模拟实验和基于热力学的土壤水多相转化模式的研究,将在冻土水文学的微观机制、尺度效应以及预测能力等方面获得新的认识,建立适合高寒山区的多尺度分布式流域水文模型,使寒区水文过程预测预报达到更高的水平。 |
其他语种文摘
|
The water feeding of main rivers in Asia is under influence by cold environment in alpine regions. The snow coverage and soil freeze affect surface condition of runoff generation of river heads. The mechanism of water- ice phase transition plays an important role to the river water supplying in cold regions. It greatly affects the water resource for large rivers in Asia,especially in the impact of global climate change. The soil freezing and thawing effects are the controlling factors of runoff change of mountainous rivers. The prediction of stream flow is of large uncertainty under the influence of climate change,which is the hotspot in the study on the global change impacting water resource. To explore the runoff change rule of river heads in Asia and predicate the water resource dynamics, one needs to know the alpine environment affecting freeze pattern of soil water,determine transformation condition and threshold of soil ice-water in mountain regions,design runoff generation models and parameters in alpine region, propose relative theories on the soil freezing-thawing and runoff generation. For these purposes,jointed stadies are necessary for the mountain field hydrological observation,simulation experiments of soil freezing and thawing in laboratory,and mode study of phase transition of soil water based on the thermodynamics. These studies will solve the key problems in micro-mechanism of cold hydrology,scale effect and predication techniques. It will help to develop multi-scale distributed hydrological models,and enhance the forecasting level for the river hydrographs in mountain regions. |
来源
|
地球科学进展
,2017,32(10):1020-1029 【核心库】
|
DOI
|
10.11867/j.issn.1001-8166.2017.10.1020.]
|
关键词
|
冻土水文
;
高原山区
;
气候变化
;
模拟预测
|
地址
|
中国科学院成都山地灾害与环境研究所, 四川, 成都, 610041
|
语种
|
中文 |
文献类型
|
综述型 |
ISSN
|
1001-8166 |
学科
|
地质学 |
基金
|
国家自然科学基金项目
|
文献收藏号
|
CSCD:6128693
|
参考文献 共
80
共4页
|
1.
刘昌明.
中国水资源现状评价和供需发展趋势分析,2001
|
被引
85
次
|
|
|
|
2.
王澄海. 40余年来中国地区季节性积雪的空间分布及年际变化特征.
冰川冻土,2009,31(2):301-310
|
被引
57
次
|
|
|
|
3.
姚檀栋. 高亚洲冰川的近期退缩及其对西北水资源的影响.
中国科学: D辑,2004,34(6):535-543
|
被引
108
次
|
|
|
|
4.
Liu S. Glacier retreat as a result of climate warming and increased precipitation in the Tarim River Basin, Northwest China.
Annals of Glaciology,2006,43(1):91-96
|
被引
7
次
|
|
|
|
5.
王根绪. 长江源区高寒生态与气候变化对河流径流过程的影响分析.
冰川冻土,2007,29(2):159-168
|
被引
34
次
|
|
|
|
6.
Wu Mousong. Experimental study on evaporation from seasonally frozen soils under various water, solute and groundwater conditions in Inner Mongolia,China.
Journal of Hydrology,2016,535:46-53
|
被引
7
次
|
|
|
|
7.
Ala Musa. Characteristics of soil freeze-thaw cycles and their effects on water enrichment in the rhizosphere.
Geoderma,2016,264:132-139
|
被引
1
次
|
|
|
|
8.
Immerzeel W W. Climate change will affect the Asian water towers.
Science,2010,328:1382-1385
|
被引
356
次
|
|
|
|
9.
Viviroli D. Mountains of the world, water towers for humanity: Typology,mapping,and global significance.
Water Resources Research,2007,43(7)
|
被引
23
次
|
|
|
|
10.
李述训. 气候持续变暖条件下青藏高原多年冻土变化趋势数值模拟.
中国科学: D辑,1996,26(4):343-347
|
被引
1
次
|
|
|
|
11.
周幼吾. 我国多年冻土的主要特征.
冰川冻土,1982,4(1):1-21
|
被引
93
次
|
|
|
|
12.
徐学祖. 土体冻结和冻胀研究的新进展??"国际地层冻结和冻结作用研讨会"论文综述.
冰川冻土,1997,19(3):280-283
|
被引
7
次
|
|
|
|
13.
石春林. 饱和土壤冻融过程中水热迁移数值模拟.
中国农业气象,1998,19(4):21-26
|
被引
2
次
|
|
|
|
14.
丁永建. 青藏高原大尺度冻土水文监测研究.
科学通报,2000,45(2):208-214
|
被引
42
次
|
|
|
|
15.
徐学祖.
冻土物理学,2001
|
被引
197
次
|
|
|
|
16.
杨梅学. 青藏高原土壤水热分布特征及冻融过程在季节转换中的作用.
山地学报,2002,20(5):553-558
|
被引
61
次
|
|
|
|
17.
Iwata Y. Influence of rain,air temperature,and snow cover on subsequent spring-snowmelt infiltration into thin frozen soil layer in northern Japan.
Journal of Hydrology,2011,401(3):165-176
|
被引
9
次
|
|
|
|
18.
Iwata Y. Comparison of soil frost and thaw depths measured using frost tubes and other methods.
Cold Regions Science and Technology,2012,71:111-117
|
被引
1
次
|
|
|
|
19.
Zhou Xiaohai. Wolfgang kinzelbach and fritz stauffer, simultaneous measurement of unfrozen water content and ice content in frozen soil using gamma ray attenuation and TDR.
Water Resource Research,2014,50(12):9630-9655
|
被引
4
次
|
|
|
|
20.
Butnor J R. Measuring soil frost depth in forest ecosystems with ground penetrating radar.
Agricultural and Forest Meteorology,2014,192:121-131
|
被引
3
次
|
|
|
|
|