Correlation of eco-hydrographic benefit and height increment of Robinia pseudoacacia stand with climatic environmental factors in Yellow River Delta Wetland of China  

黄河三角洲湿地刺槐林水文效益和生长量与气候因子的关系(英文)

作　　者：高鹏[1] 杨慧玲[1] 张光灿[1] 周泽福 

机构地区：[1]山东农业大学林学院/农业生态与环境重点实验室,泰安271018

出　　处：《Journal of Forestry Research》2008年第3期215-218,共4页林业研究（英文版）

基　　金：the National "11th Five Year" Plan of Science and technology (2006BAD26B06,2006BAD03A1205) ;Ecological Restore Project of Water Resources Ministry of China (2006-2008)

摘　　要：The relationship between eco-hydrographic benefit of forest vegetation and climatic environmental factors is one of the focuses in the research on environmental protection and ecosystem countermeasures in Wetland. The runoff, sediment and soil moisture rate dynamics in Robinia pseudoacacia plantation and its clearcut area were investigated in the natural runoff experiment plots in Yellow River Delta Wet- land, Shandong Province, China. The correlation of height increment ofR. pseudoacacia with nine climate factors such as light, water, heat, etc. was analyzed by stepwise regression analysis. The results showed that the amounts of runoff and sediment in clearcut area of R. pseudoacacia were 53.9%-150.8% and 172.8%-387.1% higher than that in Robinia pseudoacacia plantation, respectively. The runoff peak value in R. pseudoacacia stand was obviously lower than that in clerarcut area, meantime, the occurrence of runoffpeak in R. pseudoacacia stand was 25 min later than in its clerarcut area. The soil moisture rates in R. pseudoacacia stand and its clearcut varied periodically with annual rainfall precipitation in both dry season and humid season. The annual mean soil moisture rate in R. pseudoacacia stand was 23.3%-25.6% higher than that in its clearcut area. Meanwhile, a regression model reflecting the correlation between the height increment of R. pseudoacacia and climatic factors was developed by stepwise regression procedure method. It showed that the light was the most important factor for the height increment ofR. pseudoacacia, followed by water and heat factors.研究湿地防护林水文生态效益与气候环境因子的响应是湿地生态保护与经营管理中的热点问题。本文通过自然降雨径流小区定位观测试验,定量研究了黄河三角洲湿地刺槐林地及其采伐迹地的产流产沙效果和土壤水分动态变化规律。刺槐林地与采伐迹地相比,一场降雨的径流量减少53.9%～150.8%,泥沙量减少172.8%～387.1%;刺槐林地降雨径流洪峰峰值比采伐迹地低0.8L·s-1,且径流洪峰值出现的时间比采伐迹地滞后25min;刺槐林地和采伐迹地土壤含水率随年内降水量变化分干湿两季,呈周期性变化,刺槐林地年平均含水率比采伐迹地高23.3%～25.6%,特别是雨季其含水率比采伐迹地高24.3%～29.8%。应用逐步回归分析理论和方法,建立了刺槐生态防护林高生长量与气候环境因子的回归模型,影响该地区刺槐林高生长的主导因子是光照因子,其次是水分因子,再次是热量因子。该项研究可为黄河三角湿地刺槐防护林的更新改造及其生态水文效益的定量评价提供科学依据。

关 键 词：Yellow River Delta wetland Robinia pseudoacacia stand Eco-hydrographic benefit height increment climatic factors 

分 类 号：S715.7[农业科学—林学] S792.27