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首页> 外文期刊>Biogeochemistry >A response to 'Changes in water colour between 1986 and 2006 in the headwaters of the River Nidd, Yorkshire, UK: a critique of methodological approaches and measurement of burning management' by Yallop et al
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A response to 'Changes in water colour between 1986 and 2006 in the headwaters of the River Nidd, Yorkshire, UK: a critique of methodological approaches and measurement of burning management' by Yallop et al

机译:Yallop等人对“ 1986年至2006年英国约克郡河尼德河上游水的颜色变化:方法学方法和燃烧管理方法的评论”的回应

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摘要

Yallop et al. (2011) question the methodological approach we used to determine the proportion of managed burning occurring in fifteen sub-catchments of the River Nidd, north-east England and our conclusion that managed moorland burning has no effect either on water colour in streams draining these sub-catchments or on the increase in water colour that has occurred over a 20 year period. In response, we defend the approach we used to determine the proportion of heather burning in these sub-catchmentsand the conclusions we drew in Chapman et al. (2010). Firstly, we would like to clarify that the aim of our paper, as stated in the introduction, was not to investigate the impact of moorland burning on catchment scale drainage water colour, but to investigate changes in stream water colour over a 20 year period and whether the timing and/or magnitude of colour release were the same for all sub-catchments. The main findings of Chapman et al. (2010) were: (i) Water colour increased in all sub-catchments,but percent increase varied considerably between sub-catchments ranging from 22 to 155%. Statistical analysis revealed that the sub-catchments could be split into two 'Types' based on water chemistry and therefore dominant source of runoff.
机译:Yallop等。 (2011)对我们用来确定在英格兰东北部的尼德河十五个小流域发生的有管理的燃烧的比例的方法学方法提出质疑,并且我们得出结论,有管理的荒地燃烧对排水这些子流的水色也没有影响-流域或20年内出现的水彩增加。作为回应,我们捍卫了用来确定这些子汇水面积中希瑟燃烧的比例的方法,以及我们在Chapman等人的研究中得出的结论。 (2010)。首先,我们想澄清一下,如引言中所述,本文的目的不是要研究荒地燃烧对流域规模排水水色的影响,而是要研究20年内溪流水色的变化,以及所有子集水区的颜色释放时间和/或幅度是否相同。 Chapman等人的主要发现。 (2010年)为:(i)所有子集水区的水色均有所增加,但子集水区的增水百分比差异很大,范围在22%至155%之间。统计分析表明,根据水化学性质,可将子汇水区分为两种“类型”,因此是径流的主要来源。

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