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首页> 外文期刊>Biogeochemistry >Concentrations and fluxes of dissolved organic carbon in an age-sequence of white pine forests in Southern Ontario, Canada
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Concentrations and fluxes of dissolved organic carbon in an age-sequence of white pine forests in Southern Ontario, Canada

机译:加拿大安大略省南部一个白松林年龄序列中溶解有机碳的浓度和通量

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摘要

We determined concentrations and fluxes of dissolved organic carbon (DOC) in precipitation, throughfall, forest floor and mineral soil leachates from June 2004 to May 2006 across an age-sequence (2-, 15-, 30-, and 65-year-old) of white pine (Pinus strobus L.) forests in southern Ontario, Canada. Mean DOC concentration in precipitation, throughfall, leachates of forest floor, Ah-horizon, and of mineral soil at 1 m depth ranged from ~2 to 7, 9 to 18, 32 to 88, 20 to 66, and 2 to 3 mg DOC L-p#, respectively, for all four stands from April (after snowmelt) through December. DOC concentration in forest floor leachates was highest in early summer and positively correlated to stand age, aboveground biomass and forest floor carbon pools. DOC fluxes via precipitation, throughfall, and leaching through forest floor and Ah-horizon between were in the range of ~1 to 2, 2 to 4, 0.5 to 3.5, and 0.1 to 2 g DOC m-po, respectively. DOC export from the forest ecosystem during that period through infiltration and groundwater discharge was estimated as ~7, 4, 3, and 2 g DOC m-po for the 2-, 15-, 30-, and 65-year-old sites, respectively, indicating a decrease with increasing stand age. Laboratory DOC sorption studies showed that the null-point DOC concentration fell from values of 15 to 60 mg DOC L-p# at 0 to 5 cm to <15 mg DOC L-p# at 50 cm. Specific ultraviolet light absorption at 254 nm (SUVA) increased from precipitation and throughfall to a maximum in forest floor and decreased with mineral soil depth. No age-related pattern was observed for SUVA values. DOC concentration in forest floor soil solutions showed a positive exponential relationship with soil temperature, and a negative exponential relationship with soil moisture at all four sites. Understanding the changes and controls of DOC concentrations, chemistry, and fluxes at various stages of forest stand development is necessary to estimate and predict DOC dynamics on a regional landscape level and to evaluate the effect of land-use change.
机译:我们确定了2004年6月至2006年5月不同年龄序列(2岁,15岁,30岁和65岁)中降水,穿透降雨,森林地面和矿质土壤渗滤液中溶解有机碳(DOC)的浓度和通量)加拿大安大略省南部的白松(Pinus strobus L.)森林。在1 m深度的降水,穿透,林地,Ah地平线和矿质土壤的渗滤液中的平均DOC浓度范围为〜2至7、9至18、32至88、20至66和2至3 mg DOC从4月(融雪后)到12月,所有四个展台的Lp#。森林地板渗滤液中的DOC浓度在初夏最高,并且与林分年龄,地上生物量和森林地板碳库呈正相关。 DOC的通量通过降雨,穿透和在林地和Ah-horizo​​n之间的淋洗介于约1-2 g,2到4、0.5到3.5和0.1到2 g DOC m-po之间。在这段时期内,对于2、15、30和65岁的地点,通过渗透和地下水排放从森林生态系统中导出的DOC估计为约7、4、3和2 g DOC m-po,分别表示随着林分龄的增加而减少。实验室DOC吸附研究表明,零点DOC浓度从0至5 cm处的15至60 mg DOC L-p#降至50 cm以下<15 mg DOC L-p#。 254 nm处的特定紫外线吸收量(SUVA)从降水和穿透处增加到林地中的最大值,并随矿质土壤深度而降低。没有观察到与年龄有关的模式的SUVA值。林地土壤溶液中的DOC浓度与土壤温度呈正指数关系,而在所有四个地点与土壤水分呈负指数关系。了解林分发育各个阶段DOC浓度,化学成分和通量的变化和控制,对于估计和预测区域景观水平上的DOC动态以及评估土地利用变化的影响是必要的。

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