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首页> 外文期刊>Hydrology and Earth System Sciences >Landscape scale patterns in the character of natural organic matter in a Swedish boreal stream network
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Landscape scale patterns in the character of natural organic matter in a Swedish boreal stream network

机译:瑞典北方河网中天然有机物特征的景观尺度格局

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摘要

This paper defines landscape-scale patterns in the character of natural organic matter (NOM) and tests for relationships to catchment soil, vegetation and topography. The drainage network of a boreal catchment, subcatchment size 0.12-78 km(2), in Northern Sweden was sampled in August 2002 during a period of stable low water flow. The NOM was characterized with UV/Vis spectroscopy, fluorescence, XAD-8 fractionation (%humic substances), gel permeation chromatography (apparent molecular weight), and elemental composition (C:N). The largest spatial variation was found for C: N, absorbance ratio, and specific visible absorptivity. The lowest variation was in fluorescence index, %humic substances and molecular retention time. The variation in total organic carbon (TOC), iron and aluminium concentration was more than twice that of C: N. Between headwater and downstream sites no significant changes were distinguished in the NOM character. At stream reaches, junctions and lakes little change (<10%) in NOM character was observed. Common factor analysis and partial least squares regression (PLS) revealed that the spatial variation in surface coverage of lakes and mires could explain some of the variation of TOC and NOM character. Our suggestion is that the mosaic of landscape elements (different amounts of water from lakes, forest soil and mires) delivers NOM with varying characteristics to a channel network that mixes conservatively downstream, with possible small changes at some stream reaches, junctions and lakes.
机译:本文定义了天然有机物(NOM)的景观尺度格局,并测试了与流域土壤,植被和地形的关系。瑞典北部的一个北汇水面积为0.12-78 km(2)的汇水面积的排水网络于2002年8月在稳定的低水流量期间进行了采样。用紫外/可见光谱,荧光,XAD-8分级分离(%腐殖质),凝胶渗透色谱(表观分子量)和元素组成(C:N)对NOM进行表征。发现C:N,吸光度比和比吸收率最大。最低的变化是荧光指数,腐殖质百分比和分子保留时间。总有机碳(TOC),铁和铝浓度的变化是C:N的两倍以上。在源头和下游站点之间,NOM特性没有明显变化。在河段,交界处和湖泊的NOM特征几乎没有变化(<10%)。公共因子分析和偏最小二乘回归(PLS)表明,湖泊和泥潭表面覆盖率的空间变化可以解释TOC和NOM特征的某些变化。我们的建议是,景观要素的镶嵌(来自湖泊,森林土壤和泥潭的不同水量)将具有不同特征的NOM输送至在下游保守混合的河道网络,在某些河流,交汇处和湖泊可能会发生微小变化。

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