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干旱区典型绿洲水库库周土壤盐分空间分异及盐岛效应

柴晨好1,2,3,王玉刚1,2*,周宏飞1,2,朱薇1,2,3,刘丽娟1,2   

  1. 1中国科学院新疆生态与地理研究所, 荒漠与绿洲生态国家重点实验室, 乌鲁木齐 830011;2中国科学院阜康荒漠生态系统国家站, 新疆阜康 831505;3中国科学院大学, 北京 100049)
  • 出版日期:2018-08-10 发布日期:2018-08-10

Spatial variability of soil salinity and “salt island” effect around oasis reservoir in arid area.

CHAI Chen-hao1,2,3, WANG Yu-gang1,2*, ZHOU Hong-fei1,2, ZHU Wei1,2,3, LIU Li-juan1,2   

  1. (1State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; 2Fukang Station of Desert of Ecology, Chinese Academy of Sciences, Fukang 831505, Xinjiang, China; 3University of Chinese Academy of Sciences, Beijing 100049, China).
  • Online:2018-08-10 Published:2018-08-10

摘要: 绿洲水库作为干旱区内陆河流域的典型水系节点,在区域农业发展中占有重要地位。为了认识农区水库对土壤盐分空间分布特征的影响,本文以三工河流域的冰湖水库和柳城子水库为例,运用经典统计分析、地统计分析和GIS相结合的方法,对比分析不同景观背景下,以水库为中心的区域土壤剖面(0~60 cm)盐分的空间变异特征。结果表明:(1)以自然景观为背景的柳城子水库各土层盐分含量(0~20 cm:20.77 g·kg-1,20~40 cm:14.96 g·kg-1,40~60 cm:16.9 g·kg-1)高于灌溉景观为主导背景的冰湖水库各土层盐分含量(0~20 cm:7.81 g·kg-1,20~40 cm:5.66 g·kg-1,40~60 cm:5.24 g·kg-1)。在土壤盐分变异性上,冰湖水库各土层盐分的变异系数CV>100%,均呈现强变异性,而柳城子水库呈现出中等变异性(10%<CV≤100%);(2)两个水库区域各层土壤盐分,均呈现中等强度空间自相关性(0.25<C0/(C0+C)<0.75),冰湖水库表层土壤盐分空间变异主要受人为活动产生的随机因素影响,但随着土层深度的增加结构性因素的影响逐渐增强,而柳城子水库土壤盐分空间变异主要受结构性因素主导;(3)农业水库区域呈现出“盐岛”效应,冰湖水库各土层非盐化土面积占主导地位,随土层深度增加,非盐化土面积逐渐增大;而柳城子水库各土层盐土面积占主导地位,随土层深度增加,盐土面积也逐渐增大。

关键词: 吉林省, 时空演变, 环境污染, 空间计量

Abstract: Oasis reservoir, a node of hydraulic system in the inland river watershed, plays an important role in transporting water in the process of regional agriculture development. We examined the effect of reservoir on soil salt accumulation with the Binghu Reservoir and Liuchengzi Reservoir in the Sangong River watershed as cases. The spatial variability of soil salinity around reservoir under two landscape types was studied by classical statistics, geostatistics and GIS. The results showed that: (1) Salt contents of soil profiles were higher in the natural landscape type around Liuchengzi Reservoir (0-20 cm: 20.77 g·kg-1; 20-40 cm: 14.96 g·kg-1; 40-60 cm: 16.9 g·kg-1) than that of Binghu Reservoir (0-20 cm: 7.81 g·kg-1; 20-40 cm: 5.66 g·kg-1; 40-60 cm: 5.24 g·kg-1) dominated by the irrigation landscape. Soil salt content showed a great variability (CV>100%) in each soil layer around the Binghu Reservoir and was moderately variable (10%<CV<100%) around the Liuchengzi Reservoir. (2) Soil salt content had a moderate spatial autocorrelation (0.25<C0/(C0+C)<0.75) around both reservoirs. Spatial dependence of soil salt content was mainly due to random factors resulted from the strong anthropogenic activities around Binghu Reservoir. The influence of structural factors gradually increased with soil depth. In contrast, the spatial variability of soil salinity was mainly induced by structural factors around Liuchengzi Reservoir. (3) There was “salt island” phenomenon around the agricultural reservoirs. Non-saline soil was a major type around the Binghu Reservoir, with the area of which increased with soil depth. However, saline soil was a dominant type around the Liuchengzi Reservoir, whose area increased with soil depth.

Key words: spatial-temporal evolution, Jilin Province., spatial econometric, environment pollution