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生态学杂志 ›› 2009, Vol. 28 ›› Issue (11): 2293-2298.

• 研究报告 • 上一篇    下一篇

干旱区不同景观单元土壤盐分的变化特征

王玉刚;郑新军;李彦**   

  1. 中国科学院新疆生态与地理研究所阜康荒漠生态站,绿洲生态与荒漠环境重点实验室,乌鲁木齐 830011
  • 出版日期:2009-11-10 发布日期:2009-11-10

Change characteristics of soil salt content in different landscape units in arid region.

WANG Yu-gang;ZHENG Xin-jun;LI Yan   

  1. Fukang Station of Desert Ecology, Key Laboratory of Oasis Ecology and Desert Environment, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
  • Online:2009-11-10 Published:2009-11-10

摘要: 针对内陆河流域空间土壤盐渍化问题,以新疆三工河流域为例,通过调查、取样分析,研究了冲洪积扇和冲洪积平原2个水文地质带上一个生长季5—10月0~10、10~20 cm土壤盐分积聚特征及其主导因素。结果表明:冲洪积扇土壤盐分含量明显低于冲洪积平原,盐分含量的变异系数均>100%,属于强变异性;灌溉景观土壤盐分的聚积在冲洪积扇和冲洪积平原相似,盐分含量均减小,而非灌溉景观的差异较大,冲洪积扇区土壤盐分含量减小,土壤盐渍化程度减弱;而冲洪积平原区土壤盐分含量升高,盐渍化程度增强。冲洪积扇区土层间盐分变化关系紧密相关(P<0.01),降雨和灌溉对盐分都具有淋洗作用,促进了盐分含量的减少;冲洪积平原区,蒸发对非灌溉景观0~10 cm土层盐分聚积起到促进作用,而10~20 cm土层盐分聚积受上层土壤盐分和地下水位共同作用。

关键词: 中国林蛙, 变态蝌蚪, pH, 盐度, 碱度, 适应性

Abstract: Aiming at the problem of soil salinization in inland river basin, a case study was conducted in the Sangong River catchment of Xinjiang, China. The characteristics and dominant affecting factors of salt accumulation in 0-10 cm and 10-20 cm soil layers in two hydro geological zones, i.e., alluvial-proluvial delta and alluvial plain, were studied in a growth season (from May to October), and the precipitation, evaporation, groundwater table, and irrigation were also taken into account. The soil salt content was obviously lower in alluvial-proluvial delta than in alluvial plain, but its coefficient of variation in the two zones was all higher than 100%, indicating a great variability. The soil salt accumulation in-irrigated landscape in the two zones had a similar decreasing trend, but that in nonirrigated landscape had greater difference, with a decreased soil salinization in alluvial-proluvial delta, and an increased soil salinization in alluvial plain. In alluvial-proluvial delta, the salt contents in 0-10 cm and 10-20 cm soil layers had a close relationship (P<0.01), and there was a clear process of salt leaching by precipitation and irrigation, leading to the decrease of soil salt content. In alluvial plain, the salt accumulation in 0-10 cm soil layer in non-irrigated landscape was promoted by evaporation, and that in 10-20 cm soil layer was co-affected by the salt content in 0-10 cm soil layer and the groundwater table.

Key words: Rana chensinensis, Abnormal tadpole, pH, Salinity, Alkalinity, Adaptability