腐殖质
环境科学
泰加语
北方的
缓冲区
磷
水文学(农业)
化学
土壤科学
环境化学
土壤水分
生态学
地质学
生物
有机化学
岩土工程
作者
Riitta Väänänen,Kaarle Kenttämies,Mika Nieminen,Hannu Ilvesniemi
出处
期刊:Boreal Environment Research
日期:2007-01-01
卷期号:12 (5): 601-609
被引量:4
摘要
Hydrological losses of phosphorus (P) from forested areas have been reported to increase after harvesting operations. An efficient method of decreasing P losses has been to leave unmanaged buffer zones along forest brooks, streams and lakes. However, the processes controlling P retention by buffer zones are still not fully understood. To assess the importance of forest humus layer in P retention a small-scale survey was carried out at three buffer zones and adjoining clear-cut areas in southern Finland. In general, the humus layer in the buffer zones adsorbed more P than in clear-cut areas and the P adsorption was strongly related to the contents of oxalate extractable iron and aluminium. However, there were indications that the P retention capacity of the humus may decrease with the length of time the clear-cut area or buffer zone has been under the impacts of clear-cutting. There may be significant seasonal changes in humus P retention, but further studies are needed for a critical evaluation of the changes in humus P adsorption between seasons and years. Nevertheless, when compared with the increase in P release after harvest in a boreal forest, the maximum P retention capacity of the humus layer was small. Therefore, the role of the forest humus layer in P retention in clear-cut areas and buffer zones may be insignificant.
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