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作 者:薛立[1] 薛晔[2] 郑卫国 傅静丹[1] 冯慧芳[1] 史小玲[1]
机构地区:[1]华南农业大学林学院,广东广州510642 [2]浙江工业大学,浙江杭州310023
出 处:《水土保持通报》2010年第1期31-34,共4页Bulletin of Soil and Water Conservation
基 金:广东省林业局资助项目"林分改造优良乡土阔叶树种筛选"(4400-F08018);佛山市科技资助项目"南亚热带松类复合生态系统研究"(2005020061)
摘 要:研究了佛山的湿地松林地表径流及可溶解性氮和磷流失的特点。结果表明,湿地松林的年径流量为16.7mm,集中在夏季。林分的地表径流量和降雨量的关系按照二项式方程变化。地表径流中氮浓度与径流量之间存在着对数关系。湿地松林的地表径流中可溶解性氮输出量为221g/(hm2.a),春季和夏季为氮流失高峰期,占可溶解性氮年流失量的80%以上。湿地松林地表径流中可溶解性磷流失量为7.0g/(hm2.a),2008年5月和6月为湿地松林的地表径流中可溶解性磷流失高峰,占该年流失量的59%。The characteristics of runoff and dissolvable nitrogen and phosphorus losses from a Pinus elliottii stand were studied in Foshan City. The annual amount of runoff from the Pinus elliottii stand was 16.7 mm, which was mainly observed in summer. The relationship between rainfall and runoff in the stand could be de- scribed by a binomial equation. A logarithmic relationship existed between runoff and N concentration. Annual dissolvable N loss from the stand was 221 g/(hm^2 · a) and in spring and summer, it reached its peak with above 80% of annual dissolvable N loss. Annual dissolvable P loss from the stand was 7.0 g/(hm^2 · a). The greatest monthly dissolvable P loss occurred in May and June, 2008, accounting 59% of its annual P loss.
分 类 号:S725[农业科学—林木遗传育种]
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