摘要
对中国南部一个常绿阔叶林的溶质输入量、输出量和积存量进行了评价。输入量和输出量随季节而变化,并与水量的变化密切相关。春季至初夏水量增大,溶质的输出量,特别是盐基阳离子,HCO_3^-和 Si 也随之增加。积累于流域中的硫(723eq/hm^2·a)可能是来源于中国西南部城市和工业区的大气污染。由于内部循环,氮主要保存于土壤中(409eq/hm^2·a)。钾的损失受到内部循环的抑制。钠在生态系中则保持不强。镁在植被中的含量很高,但由风化的产出量也多。大气的钙输人量导致高的钙输出量。
Solute input and output budgets were evaluated for an evergreen broad-leaved forest in sothern China.Inputs and outputs varied with season,and were linked to water flux patterns.During spring to early summer with high water flow,solute output increased especially for base cations,HCO_3^-,and Si. The sulfur that accumulated in the watershed(723 eq/ha/y)were probably derived from atmospheric sources in the urban and industrial areas in the southwestern part of Chia.Considering internal cycling, nitrogen was highly retained in the soil(409 eq/ha/y).Loss of K was inhibited by internal cycling.Sodi- um was not held tightly in this ecosystem.For Mg,content in vegetation was high,but production by weathering was also important.Atmospheric Ca input contribute to higher output of Ca.
出处
《资源科学》
CSSCI
CSCD
北大核心
2001年第z1期68-76,共8页
Resources Science
关键词
大气沉降
元素积存量
养分循环
亚热带森林
流域
Atmospheric deposition
Element budget
Nutrient cycling
Subtropical forest
Watershed