酸性沉降与日本森林衰退  

Acid Deposit and Forest Decline in Japan

作　　者：郭玉文[1,2] 孙翠玲[1,2] 宋菲 

机构地区：[1]中国林科院森环所 [2]林业部规划院

出　　处：《世界林业研究》1997年第1期52-56,共5页World Forestry Research

摘　　要：酸性沉降物包括干沉降物和湿沉降物，日本把ｐＨ值低于５．６的降水称为酸性降水。近年来，日本降雨的ｐＨ值为３．８０～５．５０。酸性沉降对森林生态系统的物质循环会产生一定的影响。人工模拟酸雨实验结果表明，ｐＨ值低于４时可减少杉木苗细根伸长和个体生长，而日本酸雨ｐＨ值多为４以上，可见酸雨直接造成杉木苗枯萎的可能性并不大，但酸雾的危害不可忽视；酸性沉降物与臭氧的协同作用越来越引起人们的关注。酸性沉降不仅对林木生长产生直接影响，而且通过土壤还对林木产生间接影响。对土壤酸化作为森林衰退可能原因之一也开展了深入研究。Acid deposits are fallen into two categories, the dry and wet. In Japan the precipitation with pH value less than 5.6 is called acid precipitation. In recent years, a lot of research has been carried out in the acid deposits related to forest decline in terms of the acid rain and matter cycling of forest ecosystem, the effects of acid deposit on forest tree growth and forest soil acidification. The experimental results of artificially simulated acid rain has shown that the elongation of fibrous roots of Cunninghamia lanceolata seedlings can be reduced if the pH value of acid rain is less than 4 even though the acid rain does not directly damage the seedlings. However,the effect of acid deposit associated with ozone is increasingly receiving more attention. The acid deposits have not only directly affected on tree growth but also indirectly through the acidification of forest soil which is probably one of the facts that cause forest decline.

关 键 词：酸性沉降 酸雨 PH值 森林衰退 

分 类 号：S718.55[农业科学—林学] X517.032.3[环境科学与工程—环境工程]