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Scientia Silvae Sinicae ›› 2012, Vol. 48 ›› Issue (4): 1-7.doi: 10.11707/j.1001-7488.20120401

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Response of Stream Water Chemistry to Rainwater Acidification in the Natural Forest Region of the Qinling Mountains

Zhang Shengli1,2,3, Liang Cuiping1,2, Jin Jianxia1,2, Qin Chao1   

  1. 1. College of Resources and Environment, Northwest A&F University Yangling 712100;2. Qinling National Forest Ecosystem Research Station Yangling 712100;3. Key Laboratory of Plant Nutrition and the Agri-Environment in Northwest China, Ministry of Agriculture Yangling 712100
  • Received:2011-04-14 Revised:2012-02-21 Online:2012-04-25 Published:2012-04-25

Abstract:

This study was conducted in the Huoditang naturally-regenerated forest, which is located at the center of the natural forest region across the southern-slope of the Qinling Mountains. Rainwater and stream water samples were collected mainly in rainy seasons in the area. The sample pH values and chemical concentrations were measured. The response of stream water chemistry to rainwater acidification in the region was studied. The results showed that long time rainwater acidification could result in reduction of pH value, Ca2+ and Mg2+ concentration in the strean water. The changes of K+, Na+ concentration of stream water were not correlated with the rainwater acidification. There was no response of Zn, Pb and Cd concentration of the stream water to rainwater acidification. The acidified rainwater did not result in the release of the heavy metals enriched in the forest soil.

Key words: Qinling Mountains, forest, water chemistry, rainwater acidification

CLC Number: