西北内陆盆地冻结-冻融期的地下水补给与损耗

郭占荣; 韩双平; 荆恩春

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西北内陆盆地冻结-冻融期的地下水补给与损耗

郭占荣, 韩双平, 荆恩春

文章导航 > 水科学进展 > 2005 > 16(3): 321-325

郭占荣, 韩双平, 荆恩春. 西北内陆盆地冻结-冻融期的地下水补给与损耗[J]. 水科学进展, 2005, 16(3): 321-325.

引用本文:

郭占荣, 韩双平, 荆恩春. 西北内陆盆地冻结-冻融期的地下水补给与损耗[J]. 水科学进展, 2005, 16(3): 321-325.

GUO Zhan-rong, HAN Shuang-ping, JING En-chun. Recharge and loss of groundwater during freezing-thawing period in inland basin, Northwestern China[J]. Advances in Water Science, 2005, 16(3): 321-325.

Citation:

GUO Zhan-rong, HAN Shuang-ping, JING En-chun. Recharge and loss of groundwater during freezing-thawing period in inland basin, Northwestern China[J]. Advances in Water Science, 2005, 16(3): 321-325.

西北内陆盆地冻结-冻融期的地下水补给与损耗

1.
厦门大学海洋与环境学院, 福建, 厦门, 361005;
2.
中国地质科学院水文地质环境地质研究所, 河北, 石家庄, 050061

基金项目: "九五"国家重点科技攻关资助项目(96-912-01-03S)

详细信息

作者简介:
郭占荣(1965- ),男,内蒙古达拉特旗人,厦门大学副教授,博士,主要从事水文地质与海洋地质方面研究.E-mail:gzr@xmu.edu.cn

中图分类号: TV211.12

Recharge and loss of groundwater during freezing-thawing period in inland basin, Northwestern China

1.
Department of Oceanography, Xiamen University, Xiamen 361005, China;
2.
Institute of Hydrogeology and Engineering Geology, CAGS, Shijiazhuang 050061, China

Funds: The study is financially supported by the National Key Technologies R & D Program of China during the 9th Five-year Plan Period(No.96-912-01-03S)

摘要: 天山北麓平原区,每年冻结过程的时间远大于融化过程。在昌吉地下水均衡试验场,选择该平原的3种代表性土壤(粉质轻粘土、细砂、砂砾石),利用地中渗透仪观测冻结冻融期的地下水补给与损耗。根据不同岩性的地下水蒸发极限深度,设计了不同的地下水埋深。在冻结期,砂砾石、细砂岩性分布地区有利于浅埋型地下水资源的保护。在冻融期,无论何种地下水埋深水平,3种岩性的地下水都获得冻融水的补给,但细颗粒岩性的补给量相对较少且存在滞后效应,相反,粗颗粒岩性更有利于地下水资源的形成。冻结期一个月的地下水最大损耗量不超过253mm(砂砾石),而冻融期一个月的地下水最大补给量高达1133mm(细砂),冻融期是年内地下水的重要补给时期。
- 地下水补给 /
- 地下水损耗 /
- 冻结冻融期 /
- 西北内陆盆地
Abstract: In the plain located in the north slope of Tianshan Mountain, early November is the beginning of the freezing period, while early March next year is the beginning of the thaw period.And the freezing period is much longer than the thaw period.In the experimentation station of the groundwater balance, located in Changji County, three kinds of soil (stony sand, fine sand and clay), which are local typical soil in the inland basins, are chosen to observe the recharge and the loss of groundwater in freezing-thaw period.According to the critical depths of groundwater loss, several kinds of groundwater table are designed for all kinds of soil.In the freezing period, where the stony sand and sand are distributed, the protection of groundwater resources is favorable In the thaw period, no matter what depth of groundwater table, the recharge occurrs for all of the three, but the recharge of the fine grained soil is relatively less and shows the delaying effect.Contrarily, the coarse grained soil is more favorable for the formation of groundwater resources.The largest loss of groundwater is not beyond 25.3 mm in one month during the freezing period(for example, stony sand), and the largest recharge is more than 113.3 mm in the same time during the thaw period(for example, fine grained sand), so the thaw period is the important period of groundwater recharge each year.
- groundwater recharge /
- groundwater loss /
- freezing-thaw period /
- inland basin in northwestern China

[1]	郭占荣,刘花台,荆恩春.西北内陆盆地潜水与土壤水转化关系研究[J].水文,2002,22(2):1-5.
[2]	郭占荣,荆恩春,聂振龙.冻结期和冻融期土壤水分运移特征分析[J].水科学进展,2002,13(3):298-302.

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西北内陆盆地冻结-冻融期的地下水补给与损耗

1. 厦门大学海洋与环境学院, 福建, 厦门, 361005;

2. 中国地质科学院水文地质环境地质研究所, 河北, 石家庄, 050061

基金项目: "九五"国家重点科技攻关资助项目(96-912-01-03S)

作者简介:
郭占荣(1965- ),男,内蒙古达拉特旗人,厦门大学副教授,博士,主要从事水文地质与海洋地质方面研究.E-mail:gzr@xmu.edu.cn

收稿日期: 2004-03-12
修回日期: 2004-05-30
刊出日期: 2005-05-25

中图分类号: TV211.12

关键词:

摘要: 天山北麓平原区,每年冻结过程的时间远大于融化过程。在昌吉地下水均衡试验场,选择该平原的3种代表性土壤(粉质轻粘土、细砂、砂砾石),利用地中渗透仪观测冻结冻融期的地下水补给与损耗。根据不同岩性的地下水蒸发极限深度,设计了不同的地下水埋深。在冻结期,砂砾石、细砂岩性分布地区有利于浅埋型地下水资源的保护。在冻融期,无论何种地下水埋深水平,3种岩性的地下水都获得冻融水的补给,但细颗粒岩性的补给量相对较少且存在滞后效应,相反,粗颗粒岩性更有利于地下水资源的形成。冻结期一个月的地下水最大损耗量不超过253mm(砂砾石),而冻融期一个月的地下水最大补给量高达1133mm(细砂),冻融期是年内地下水的重要补给时期。

English Abstract

Recharge and loss of groundwater during freezing-thawing period in inland basin, Northwestern China

1. Department of Oceanography, Xiamen University, Xiamen 361005, China;

2. Institute of Hydrogeology and Engineering Geology, CAGS, Shijiazhuang 050061, China

Funds: The study is financially supported by the National Key Technologies R & D Program of China during the 9th Five-year Plan Period(No.96-912-01-03S)

Received Date: 2004-03-12
Rev Recd Date: 2004-05-30
Publish Date: 2005-05-25

Keywords:

Abstract: In the plain located in the north slope of Tianshan Mountain, early November is the beginning of the freezing period, while early March next year is the beginning of the thaw period.And the freezing period is much longer than the thaw period.In the experimentation station of the groundwater balance, located in Changji County, three kinds of soil (stony sand, fine sand and clay), which are local typical soil in the inland basins, are chosen to observe the recharge and the loss of groundwater in freezing-thaw period.According to the critical depths of groundwater loss, several kinds of groundwater table are designed for all kinds of soil.In the freezing period, where the stony sand and sand are distributed, the protection of groundwater resources is favorable In the thaw period, no matter what depth of groundwater table, the recharge occurrs for all of the three, but the recharge of the fine grained soil is relatively less and shows the delaying effect.Contrarily, the coarse grained soil is more favorable for the formation of groundwater resources.The largest loss of groundwater is not beyond 25.3 mm in one month during the freezing period(for example, stony sand), and the largest recharge is more than 113.3 mm in the same time during the thaw period(for example, fine grained sand), so the thaw period is the important period of groundwater recharge each year.

郭占荣, 韩双平, 荆恩春. 西北内陆盆地冻结-冻融期的地下水补给与损耗[J]. 水科学进展, 2005, 16(3): 321-325.

引用本文:

郭占荣, 韩双平, 荆恩春. 西北内陆盆地冻结-冻融期的地下水补给与损耗[J]. 水科学进展, 2005, 16(3): 321-325.

GUO Zhan-rong, HAN Shuang-ping, JING En-chun. Recharge and loss of groundwater during freezing-thawing period in inland basin, Northwestern China[J]. Advances in Water Science, 2005, 16(3): 321-325.

Citation: