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Dynamics of concentrations of total organic carbon in Estonian streams, 1992-2007

机译:Etonian流中总有机碳浓度的动态,1992-2007

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Human activities have begun to transform northern peatlands into global sources of dissolved organic carbon (DOC). In Estonia, there are 10,091 km~2 of peatlands, constituting 22.3% of the country's total area. The increasing number of drought days during the last 50 years, which constitutes a threat of an increased flux of dissolved carbon, has also been observed in Estonia. The aim of the current study was to explain organic carbon trends in Estonian streams during the period 1992-2007. The national environmental monitoring programme initiated the measurement of total organic carbon (TOC) in Estonian streams in 1998. We reconstructed the earlier concentrations of TOC through the link with permanganate oxygen consumed (POC). The TOC and POC data of 64 weirs was studied. The determination coefficients between TOC and POC were over 0.75 for the nine North Estonian streams (Kasari, Vihterpalu, Vaana, Keila, Pirita, Jagala, Pudisoo Valgejogi and Loobu). The R~2 values in the rest of the sampled weirs were below 0.7. Likewise, the temporal trend of both TOC and POC data was insignificant. In northern Estonia, a weak but significant (R~2=0.09, p<0.05) rising trend in TOC concentrations was observed. This may have resulted from the high percentage of peatlands and more calcareous soils in northern Estonian catchments. The trend corresponds with earlier data from northern catchments, being influenced by the effects of global warming and/or changes in the chemistry of atmospheric deposition, and demonstrating a complex positive feedback in the global C cycle.
机译:人类的活动已经开始将北部泥土转化为全球溶解有机碳源(DOC)。在爱沙尼亚,泥炭地有10,091公里〜2,占该国总面积的22.3%。在过去50年期间,越来越多的干旱日期,这在爱沙尼亚也观察到溶解碳通量增加的威胁。目前研究的目的是在1992 - 2007年期间解释爱沙尼亚流的有机碳趋势。国家环境监测方案于1998年开始测量爱沙尼亚溪流的总有机碳(TOC)。我们通过与含有高锰酸盐氧气(POC)的联系重建了较早的TOC浓度。研究了64堰的TOC和POC数据。 TOC和PoC之间的确定系数为九个北爱安炎溪流的0.75(Kasari,Vihterpalu,Vaana,Keila,Pirita,Jagala,Pudisoo Valgejogi和Loobu)。其余的抽样堰中的R〜2值低于0.7。同样,TOC和POC数据的时间趋势是微不足道的。在爱沙尼亚北部,观察到TOC浓度的弱但显着(R〜2 = 0.09,P <0.05)趋势上升。这可能是由爱沙尼亚北部地区的高百分比和更多钙质土壤中的泥炭地。该趋势与来自北方集水区的早期数据相对应,受到大气沉积化学化学的全球变暖和/或变化的影响,并在全球C循环中展示复杂的正反馈。

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