主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

气象与环境学报

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辽河三角洲主要植被类型土壤水盐含量研究

吕国红1, 2, 4;周莉3;贾庆宇1;王笑影1;戴萍5   

  1. 1. 中国气象局沈阳大气环境研究所,沈阳 110016;2. 中国科学院沈阳应用生态研究所,沈阳 110016;3. 中国科学院北京植物研究所植被数量生态学重点实验室,北京 100093;4. 中国科学院 研究生院,北京 100039;5. 沈阳区域气候中心,辽宁 沈阳 110016;)
  • 收稿日期:2010-11-08 修回日期:2010-11-22 出版日期:2010-12-29 发布日期:2010-12-29

Study on soil water and salt contents for main vegetation communities in the Liaohe Delta

LV Guo-hong1,2,4;ZHOU Li3;JIA Qing-yu1;WANG Xiao-ying1;DAI Ping5
  

  1. 1.Institute of Atmospheric Environment, China Meteorological Administration, Shenyang 110016, China; 2. Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; 3. Laboratory of Quantitative Vegetation Ecology, Institute of Botany, the Chinese Academy of Sciences, Beijing 100093, China; 4. Graduate School of the Chinese Academy of Sciences, Beijing 100039, China; 5. Shenyang Regional Climate Center, Shenyang 110016, China)
  • Received:2010-11-08 Revised:2010-11-22 Online:2010-12-29 Published:2010-12-29

摘要: 基于不同植被类型,探讨辽河三角洲土壤的水盐状况,研究土壤全盐与土壤含水量及土壤pH值之间的关系。结果表明:辽河三角洲植被类型不同,土壤盐分、土壤含水量及土壤pH值明显不同。不同土层裸滩土壤全盐量均较高,小叶杨最低。翅碱蓬、紫花苜蓿、芦苇和柽柳作为盐生植被,对土壤含盐量影响较大。不同土层小叶杨土壤含水量均较低。裸滩、翅碱蓬及芦苇受潮汐影响较大,土壤含水量差异较大。调查区土壤pH值偏碱性,变化范围为7.30—8.97。土壤全盐、土壤含水量及土壤pH值之间总体呈显著相关,可见土壤含水量和pH值是显著影响土壤全盐量的重要因素。

关键词: 土壤全盐, 土壤含水量, 土壤pH值, 辽河三角洲

Abstract: Soil water and salt contents for main vegetation communities were analyzed and the relationships among soil total salt content, soil water content and soil pH were discussed in different soil layers in the Liaohe Delta. The results show that soil total salt content, soil water content and soil pH are obviously different for different vegetation communities in different soil layers. Soil total salt content is the highest in bare soil and the lowest in forest (Populus simonii) soil for different soil layers. The effects of halophytic vegetation on soil salt content are significant, such as seepweed (Suaeda salsa), alfalfa (Medicago sativa), reed (Phragmites communis) and willow (Tamarix chinensis). Soil water content is lower in forest (Populus simonii) soil for different soil layers. The effects of tide on bare soil, seepweed community and reed community are obvious, so the differences of soil water contents among them is also significant. Soil pH is 7.30-8.97 in study area. In general, soil total salt content is significantly related with soil water content and soil pH, which indicates that soil water content and soil pH are important factors influencing soil total salt content.

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