干旱区研究 ›› 2023, Vol. 40 ›› Issue (12): 1898-1906.doi: 10.13866/j.azr.2023.12.03 cstr: 32277.14.j.azr.2023.12.03

• 水土资源 • 上一篇    下一篇

石羊河流域水文与水资源特征及其对沙漠化影响

柴会霞1(),安志山2(),潘加朋2,3   

  1. 1.甘肃省水利水电勘测设计研究院有限责任公司甘兰设计院,甘肃 兰州 730000
    2.中国科学院西北生态环境资源研究院敦煌戈壁荒漠生态与环境研究站,甘肃 兰州 730000
    3.中国科学院大学,北京 100049
  • 收稿日期:2023-06-04 修回日期:2023-07-06 出版日期:2023-12-15 发布日期:2023-12-18
  • 作者简介:柴会霞(1979-),女,高级工程师,主要从事水资源与水利工程规划研究. E-mail: 565003792@qq.com
  • 基金资助:
    甘肃省自然科学基金(22JR5RA066);国家自然科学基金(42171015)

Characteristics of hydrological and water resources in the Shiyang River Basin and their effects on land desertification

CHAI Huixia1(),AN Zhishan2(),PAN Jiapeng2,3   

  1. 1. Design Institute of Ganlan, Gansu Water Conservancy and Hydropower Survey, Design and Research Institute Co. Ltd., Lanzhou 730000, Gansu, China
    2. Dunhuang Gobi and Desert Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, Gansu, China
    3. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2023-06-04 Revised:2023-07-06 Published:2023-12-15 Online:2023-12-18

摘要:

通过分析石羊河流域降水量、径流量、输沙量等水文参数,统计沙漠化土地面积变化,揭示流域水文与水资源特征和沙漠化土地变化规律,为流域沙漠化土地防治提供科学依据与理论基础。研究表明:2005—2021年,石羊河流域降水量呈增加趋势,但变率大且维持在较低水平,多年平均降水量仅234.70 mm;1993—2004年,蔡旗水文站年径流量下降,年输沙量上升;1999—2021年,杂木寺水文站年径流量增加,年输沙量减小;2005—2021年,石羊河流域水资源总量年均减少0.24×108 m3,多年平均用水量和耗水量分别为24.70×108 m3和17.07×108 m3,且农业和林果产业用水量和耗水量偏高。1975—2014年流域沙漠化土地总面积减小,表明区域生态治理工程取得一定成效,但不同时段和不同沙漠化类型土地变化仍有较大差异。

关键词: 石羊河流域, 水文特征, 水资源, 土地沙漠化

Abstract:

In this article, using the parameters of hydrological, water resources, and the desertification area of the Shiyang River basin in different periods, the basin hydrology, water resources, desertification, and its changes in the relationship between them were quantitatively studied. It provides the data and the theoretical basis for hydrological, water resource features, and land desertification in this area. The research showed that although the precipitation in the Shiyang River basin had increased from 2005 to 2021, the variability was large and remained at a low level, with an average annual precipitation of only 234.70 mm. From 1993-2004, the annual precipitation at the Caiqi hydrological station reduced, whereas the annual sediment transport increased. The annual precipitation at the Zamusi hydrological station increased from 1999 to 2021, whereas the annual sediment discharge decreased. From 2005 to 2021, the total amount of water resources in the Shiyang River basin decreased by 0.24×108 m3 ·a-1, but water consumption and water consumption remained at high levels of 24.70× 108 m3 and 17.07×108 m3, with high water consumption and consumption in agriculture, forestry, and fruit industries, exacerbating the irrationality of water resource utilization in the basin. From 1975 to 2014, the total area of desertified land in the basin reduced, but the land changes in different periods and desertification types remained quite different, and the situation of desertification prevention and control in the basin was still grim.

Key words: Shiyang River Basin, hydrological characteristics, water resources, land desertification