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首页> 外文期刊>Canadian Journal of Forest Research >Relation of soil-, surface-, and ground-water distributions of inorganic nitrogen with topographic position in harvested and unharvested portions of an aspen-dominated catchment in the Boreal Plain
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Relation of soil-, surface-, and ground-water distributions of inorganic nitrogen with topographic position in harvested and unharvested portions of an aspen-dominated catchment in the Boreal Plain

机译:北方平原白杨为主集水区收获和未收获部分中无机氮在土壤,地表和地下水中的分布与地形位置的关系

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摘要

Spatial distributions of soil extractable nitrate (NO_3) and ammonium (NHJ) concentrations were related to surface- and ground-water NO_3 and NHJ concentrations in harvested and forested sections of a catchment dominated by trembling aspen (Populus tremuloides Michx.) in the subhumid boreal forest of Alberta, Canada. NO3 and NH^ concentrations in soils varied spatially throughout the catchment and were larger in surface soils than in subsurface soils. Spatial distributions of soil inorganic nitrogen(N) concentrations were not explained by the harvested versus the unharvested condition; heterogeneity was instead related to topographic position. NO_3 concentrations in both surface and subsurface soils were largest in ephemeral draws and wetlands. NH_4~+ concentrations in subsurface soils were largest in ephemeral draws and wetlands, but this pattern was not apparent for surface soils. Soil NO_3 and NH^ availability and surface- and ground-water NO_3 and NH^ concentrations reflected soil NO_3 and NH_4~+ concentrations. N-rich surface soils in both forested and harvested areas have a large potential for releasing N to surface waters. This study indicates that even though topography is subtle in this catchment, topographic position and its soil moisture relations, along with vegetation demand, can influence N transformation and transport in both forested and harvested portions of the Boreal Plain landscape.
机译:在半湿润的北方地区,以干旱的白杨(Populus tremuloides Michx。)为主的流域的采伐区和林区,土壤可提取硝酸盐(NO_3)和铵盐(NHJ)的空间分布与地表水和地下水中的NO_3和NHJ浓度有关。加拿大艾伯塔省的森林。整个集水区土壤中的NO3和NH3浓度在空间上变化,并且表层土壤中的NO3和NH2浓度高于地下土壤。收获与未收获条件不能解释土壤无机氮(N)浓度的空间分布。相反,异质性与地形位置有关。在短暂的抽水带和湿地中,表层和地下土壤中的NO_3浓度最高。在短暂抽水和湿地中,地下土壤中的NH_4〜+浓度最大,但对于表层土壤,这种模式并不明显。土壤NO_3和NH ^的有效性以及地表水和地下水NO_3和NH ^的浓度反映了土壤NO_3和NH_4〜+的浓度。森林和收获地区的富氮表层土壤都有很大的潜力将氮释放到地表水中。这项研究表明,尽管该流域的地形微妙,但地形位置及其与土壤的水分关系以及植被需求,都可以影响北方平原森林和采伐部分的氮素转化和运输。

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