首页> 外文期刊>Geoderma: An International Journal of Soil Science >Long-term landscape - land use interactions as explaining factor for soil organic matter variability in Dutch agricultural landscapes
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Long-term landscape - land use interactions as explaining factor for soil organic matter variability in Dutch agricultural landscapes

机译:长期景观-土地利用相互作用是荷兰农业景观中土壤有机质变异性的解释因素

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The present-day land use pattern is often used for estimating soil organic matter pools. Although the effect of historical land use on soil organic matter (SOM) pools is often recognized, this factor is never accounted for in large-scale SOM inventories. We assessed if an inventory of long-term landscape management can be used to improve estimates of landscape-scale SOM variability for a 60 km(2) case study in the northern Dutch sand area. We hypothesize that soil, present-day and historical land use and their interactions can explain the bulk of SOM variability at multiple scales. Actual SOM data from a 1:10.000 soil inventory of the study area were used to test this hypothesis. Land use history (1780-2000) was reconstructed using topographic maps and land use databases. Potential explaining factors for SOM contents were analysed. Linear models were used to characterize SOM variability at 50 m, 200 m and 500 m resolutions. Soil characteristics like loam content (R-2=0.25), median sand grain size (R-2=0.20) or soil classification (R-2=0.23) can partly explain total SOM variability. Present-day land use only explains 2% of SOM variability. Historical land use patterns explain a much larger part of the total SOM variability (R-2=0.14 for land use patterns in 1780 and R2=0.20 for land use patterns in 1850). At 50 m resolution, SOM contents can be best explained with soil and land use history factors (R-2=0.28). At 200 m resolution,soil and groundwater factors yileld the best model (R-2=0.42) while at 500 m resolution a model including soil, groundwater and historical land use performs best (R-2=035). We conclude that land use history data can significantly improve SOM inventories at multiple scales. Especially at detailed scales it can improve insight in both SOM pool size and origin of SOM variability. As land use history of the Netherlands is relatively well documented, we expect that an improvement of national SOM pool estimates is feasible. (C) 2008 Elsevier B.V. All rights reserved.
机译:当前的土地利用模式通常用于估算土壤有机质库。尽管人们常常认识到历史土地使用对土壤有机质(SOM)库的影响,但是在大规模SOM清单中从来没有考虑到这一因素。我们评估了荷兰北部沙子地区60 km(2)案例研究中是否可以使用长期景观管理清单来改善景观规模SOM变异性的估计。我们假设土壤,当前和历史土地用途及其相互作用可以解释多种尺度下大量的SOM变异性。来自研究区域的1:10.000土壤清单的实际SOM数据用于检验此假设。使用地形图和土地使用数据库重建了土地使用历史(1780-2000年)。分析了SOM含量的潜在解释因素。线性模型用于表征在50 m,200 m和500 m分辨率下的SOM变异性。土壤特征如壤土含量(R-2 = 0.25),中值沙粒尺寸(R-2 = 0.20)或土壤分类(R-2 = 0.23)可以部分解释总的SOM变异性。目前的土地用途只能解释SOM变异的2%。历史土地使用模式解释了总SOM变异的很大一部分(1780年土地使用模式的R-2 = 0.14,1850年土地使用模式的R2 = 0.20)。在50 m分辨率下,SOM含量可以用土壤和土地使用历史因素(R-2 = 0.28)进行最好的解释。在200 m分辨率下,土壤和地下水因子是最佳模型(R-2 = 0.42),而在500 m分辨率下,包括土壤,地下水和历史土地利用的模型效果最佳(R-2 = 035)。我们得出结论,土地使用历史数据可以从多个方面显着改善SOM库存。特别是在详细规模上,它可以提高对SOM库大小和SOM变异性来源的了解。由于荷兰的土地使用历史记录相对完整,因此我们希望对国家SOM池估算进行改进是可行的。 (C)2008 Elsevier B.V.保留所有权利。

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