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Modelling the impact of changing atmospheric pollution levels on limestone erosion rates in central London, 1980-2010

机译:模拟1980-2010年伦敦市中心大气污染水平变化对石灰石侵蚀速率的影响

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摘要

Decadal limestone erosion rates from a 30-year study of St Pauls Cathedral, London are compared with recession rates derived from applying Lipfert's and Tidblad's dose-response functions to the available rainfall and sulphur dioxide data from central London. Comparison of the measured erosion rates and the dose-response function derived recession rates shows consistently higher loss for the measured erosion rates, between 49 and 35 microns per year for measured rates as opposed to 15-12 microns per year for derived rates. Measured erosion rates were 3.33 times as high as derived recession rates towards the start of the 30 year measurement period, falling to almost 2.75 times by the 2000s. Analysis of the disparity suggests that, despite the magnitude of the differences between the two methods, they both record the same patterns of decline in erosion rates as sulphur dioxide levels decline. The disparity may result from using a common index of erosion, loss of height, to express the outcomes of two different measurement systems quantifying surface loss in different ways.
机译:将伦敦圣保罗大教堂进行的为期30年的研究得出的十年代石灰石侵蚀率与将Lipfert和Tidblad的剂量反应函数应用于伦敦市中心的可用降雨和二氧化硫数据得出的衰退率进行了比较。测得的腐蚀速率与剂量响应函数得出的衰退速率的比较表明,测得的腐蚀速率始终具有较高的损耗,测量速率的损失在每年49至35微米之间,而衍生速率的损失在每年15-12微米之间。在30年测量期开始时,测得的侵蚀率是衍生衰退率的3.33倍,到2000年代下降到近2.75倍。对差距的分析表明,尽管两种方法之间的差异很大,但它们都记录了随着二氧化硫水平下降侵蚀率下降的相同模式。这种差异可能是由于使用侵蚀的共同指标,高度损失来表示的两种不同测量系统以不同方式量化表面损失的结果。

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