School of Applied Science, Cranfield University, Cranfield, Bedfordshire, MK43 0AL, UK.
Sci Total Environ. 2010 Nov 15;408(24):6179-91. doi: 10.1016/j.scitotenv.2010.08.038.
Increasing DOC concentrations in surface waters have been observed across parts of Europe and North America over the past few decades. Most proposed explanations for these widespread trends invoke climate change or reductions in sulphate deposition. However, these factors do not seem apposite to explain either the fine-scale (within kilometres) or regional-scale spatial variation in DOC concentrations observed across the UK. We have reconstructed DOC concentrations and land use for one North Pennine and five South Pennine catchments (UK), located in three discrete areas, over the last four decades. Rainfall, temperature and sulphate deposition data, where available, were also collated and the potential influence of these factors on surface water DOC concentrations was assessed. Four of the six catchments examined showed highly significant (p<0.001) increases (53-92%) in humic coloured DOC (hDOC) concentrations in drainage waters over the period 1990-2005. Changes in temperature and sulphate deposition may explain 20-30% of this trend in these four catchments. However, the rapid expansion of new moorland burn on blanket peat can explain a far greater degree (>80%) of the change in hDOC. Far smaller increases in hDOC (10-18%) were identified for the two remaining catchments. These two sites experienced similar changes in sulphur deposition and temperature to those that had seen largest increases in DOC, but contained little or no moorland burn management on blanket peat. This study shows that regional-scale factors undoubtedly underlie some of the recent observed increases in drainage humic coloured DOC. However, changes in land management, in this case the extensive use of fire management on blanket peat, are a far more important driver of increased hDOC release from upland catchments in some parts of the UK. It suggests that the recent rapid increase in the use of burning on blanket peat moorland has implications for ecosystem services and carbon budgets.
在过去几十年中,人们观察到欧洲和北美的部分地区地表水 DOC 浓度不断增加。对于这些广泛的趋势,大多数提出的解释都涉及气候变化或硫酸盐沉积减少。然而,这些因素似乎都不适用于解释在英国观察到的 DOC 浓度的细尺度(在几公里内)或区域尺度的空间变化。我们重建了过去四十年中一个北奔宁山脉和五个南奔宁山脉流域(英国)的 DOC 浓度和土地利用情况,这些流域位于三个不同的地区。还收集了可用的降雨量、温度和硫酸盐沉积数据,并评估了这些因素对地表水 DOC 浓度的潜在影响。在所研究的六个流域中,有四个流域(53-92%)的排水中腐殖质有色 DOC(hDOC)浓度在 1990-2005 年期间呈现出非常显著的(p<0.001)增加。这四个流域中,温度和硫酸盐沉积的变化可能解释了这一趋势的 20-30%。然而,新的荒地火烧在覆盖泥炭上的迅速扩张可以解释 hDOC 变化的更大程度(>80%)。对于另外两个流域,hDOC 的增加幅度要小得多(10-18%)。这两个地点的硫沉降和温度变化与那些 DOC 增加最大的地点相似,但在覆盖泥炭上几乎没有或没有荒地火烧管理。本研究表明,区域尺度的因素无疑是最近观察到的排水中腐殖质有色 DOC 增加的部分原因。然而,土地管理的变化,在这种情况下是广泛使用火烧管理覆盖泥炭,是英国某些地区高地流域 hDOC 释放增加的一个更为重要的驱动因素。这表明,最近在覆盖泥炭荒地火烧的广泛使用对生态系统服务和碳预算产生了影响。