摘要
In order to study hydrochemical characteristics and ion transfer of annual rainfall of Betula platyphylla secondary forest,water samples of rainfall,throughfall,stemflow,litter infiltration water and slope runoff of Betula platyphylla secondary forest in the early growth stage,fastgrowing stage and growth decline stage in Shanjiankou watershed of Xiaowutai Mountain and nine indexes of pH,Ca^2+,Mg^2+,K+,Na+,Zn^2+,Mn^2+,Fe^2+ and Cu^2+ were determined.The results showed that:①The annual rainfall was weakly alkaline,and the ion concentration in different stages was obviously different.According to the ratio of the maximum concentration to the minimum concentration of the same ion,the rank was Mg^2+ > Mn^2+ >Na+ > K+ > Ca^2+ > Cu^2+ > Fe^2+ > Zn^2+.②Compared with the rainfall in the same period,in the early growth stage,Mg^2+,Mn^2+,Na+,K+,Ca^2+,Fe^2+ and Zn^2+ showed leaching loss in each distribution process.In the fastgrowing stage,Ca^2+,Mn^2+ and Fe^2+ showed leaching loss in each distribution process;Mg^2+ showed absorption,Na+ showed leaching loss in slope runoff and showed absorption in other process.K+ showed leaching loss in stemflow and showed absorption in other process.Zn^2+ showed absorption in stemflow and slope runoff and showed a little leaching loss in other process.In the late growth stage,Ca^2+,Mg^2+,Zn^2+,Mn^2+ and Fe^2+ showed leaching loss in each distribution process;Na+ and Cu^2+ showed absorption;K+ showed absorption in stemflow and showed leaching loss in other process.Most of the rainfall and metal ions in Betula platyphylla secondary forest were intercepted by litter layer.
基金
Sponsored by Subsidy Project of Operation of Forestry Science and Technology Innovation Platform(2017-LYPTDW-004).
