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Comparison of impacts of human activities and climate change on water quantity and quality in Finnish agricultural catchments

机译:人类活动和气候变化对芬兰农业流域水量和水质的影响比较

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摘要

We studied the influence of human activities and climate change on water quantity and quality. Human activities included methods of agricultural policy, i.e. land use and management practices. Finland started to follow EU's agricultural policy in 1995. In this study our main objective was to find out whether the original targets of the Finnish Agri-Environmental Programme (FAEP) were achieved. We analyzed trends in discharge, water quality and climate parameters in 37 years long time-series in two catchments. We focused on the suspended sediment and phosphorus concentrations and loads, the main interests to FAEP. We found an increasing trend in mean annual temperature, especially in spring and late summer-early autumn. There was no statistical significant change in annual runoff. Increasing winter runoff in the other catchment could be explained by the increased number of days when temperature was above zero degrees making snowmelt possible. In this area high potential sediment delivery occurred in early winter. FAEP succeeded in decreasing the suspended sediment load by reduced tillage and wintertime vegetation cover. In controlling the phosphorus loads FAEP succeeded only in the catchment with erosion sensitive soils. In the catchment where soils were less sensitive for erosion increase in the dissolved reactive phosphorus load exceeded the benefits of the reduced particulate phosphorus load. Climate change may increase the suspended sediment load by increasing winter runoff. Even then, instead of decreasing the suspended sediment loads FAEP should rather focus on dissolved nutrients as they cause eutrophication in receiving waters.
机译:我们研究了人类活动和气候变化对水量和水质的影响。人类活动包括农业政策方法,即土地使用和管理实践。芬兰于1995年开始遵循欧盟的农业政策。在这项研究中,我们的主要目标是查明是否实现了芬兰农业环境计划(FAEP)的最初目标。我们分析了两个流域37年长时间序列中的排放,水质和气候参数趋势。我们关注悬浮悬浮物和磷的浓度和负荷,这是FAEP的主要兴趣所在。我们发现年平均气温呈上升趋势,尤其是在春季和夏末至初秋。年径流量没有统计上的显着变化。其他流域冬季径流增加的原因可能是温度高于零度时增加融雪的天数。在该地区,初冬发生了大量潜在的泥沙输送。 FAEP通过减少耕种和冬季植被覆盖,成功减少了悬浮泥沙负荷。在控制磷负荷方面,FAEP仅在对侵蚀敏感的土壤流域中取得了成功。在土壤对侵蚀较不敏感的流域,溶解性活性磷负荷的增加超过了降低颗粒状磷负荷的好处。气候变化可能会通过增加冬季径流量来增加悬浮的泥沙负荷。即使这样,FAEP还是要减少溶解的营养物,而不是减少悬浮的沉积物负荷,因为它们会导致接收水中的富营养化。

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