红壤小流域不同利用方式氮磷流失特征研究  

Losses of nitrogen and phosphorus under different land use patterns in small red soil watershed

作　　者：袁东海[1] 王兆骞[1] 陈欣[1] 郭新波[1] 张如良 

机构地区：[1]浙江大学农业生态研究所,杭州310029 [2]浙江省兰溪市水土保持监督站,浙江兰溪321100

出　　处：《生态学报》2003年第1期188-198,共11页Acta Ecologica Sinica

基　　金：国家自然科学基金重点资助项目 ( 30 0 30 0 30 )~~

摘　　要：从红壤小流域坡地资源合理利用和保护的角度研究了不同利用方式土壤氮、磷流失的特征 ,结果表明 :恢复保护性植被的试验区 3,由于其水土流失量最低 ,氮、磷流失量最小。侵蚀严重的试验区 5 ,由于水土流失量最大 ,磷的流失量最大 ,但其有效磷、水溶性磷及氮素流失量低于不注重水土资源保持经营利用的试验区 1、注重水土保持措施的试验区 2和试验区 4。由于采用了水土保持综合农林措施 ,有效地减轻了水土流失 ,试验区 2和试验区 4的土壤氮、磷流失量明显小于试验区 1土壤氮、磷流失量 ,红壤小流域不同利用方式中水土保持综合措施能有效地控制土壤养分流失。2 0 0 0年不同试验区土壤氮、磷的流失主要集中于 5、6及 8月份 ,其流失量占全年氮、磷流失量的 90 %以上 ,这与当地的降雨季节性分配特征有关。土壤氮、磷的坡面流失方式为推移质流失和径流流失 ,磷的流失形态主要为泥砂结合态 ,约占总磷流失量的70 %以上。除试验区 3以外 ,其它试验区泥沙结合态氮素的流失量大于水溶态氮素流失量。Soil erosion is very significantly serious throughout China, which covers 1.80 million km2. In red soil region of southern China, soil erosion also occurred seriously with area of 0.80 million km2. Soil erosion, which causes river silted, floods, nutrient loss, water pollution, soil and land productivity degradation, has negatively impacted on sustainable agriculture development. A lot of reports on soil erosion were presented focusing on simulation based on single factor treatment. Soil erosion research on watershed scale by adopting comprehensive approaches is poor reported. Reports aim to clarify soil erosion process and the approach to develop a comprehensive farming system in some watersheds were little presented. In this paper soil erosion and nutrient loss in Jiangjiatang micro-watershed located in Lanxi City in Zhejiang Province were studied. The micro-watershed is located in west of central Zhejiang Province, at the north of Jinqu Basin and upper Qianjiang River. It is characterized by monsoon climate in a subtropical zone. Annual precipitation there is about 1400~1600mm, mainly occurred in the period during April to August. The annual mean temperature is round 17.7℃ and cumulative temperature of more than 10℃ is around 5600℃. Soil in the micro-watershed belongs to red soil, being zonal soil originating from Q 2, and the land with this soil is mostly sloped with a relative altitude of about 34m. The micro-watershed for the experiment is about 321100m2, and 194900 m2 of it is sloped, 126200 m2 is riverside land. Five experimental catchments were set up according to the naturally canal and gully systems. Each experimental catchment has respectively independent canal and gully system. This micro-watershed with five catchments was exploited and utilized in 1992. The patterns of land utilization were described as follows. Catchment 1, it was an extensive land use area with 43400 m2 where land is nearly barren and covered with few naturally grown brushwood and short bamboo (Bambusa) on the upper par

关 键 词：红壤小流域 利用方式 氮磷流失特征 坡地利用 

分 类 号：S158[农业科学—土壤学]