Department of Earth and Environmental Sciences, KU Leuven, Celestijnenlaan 200E Box 2411, 3001 Leuven, Belgium.
Department of Earth and Environmental Sciences, KU Leuven, Celestijnenlaan 200E Box 2411, 3001 Leuven, Belgium.
Sci Total Environ. 2017 Jul 1;589:153-164. doi: 10.1016/j.scitotenv.2017.02.116. Epub 2017 Mar 1.
The soil organic carbon (SOC) stock is an important indicator in ecosystem service assessments. Even though a considerable fraction of the total stock is stored in the subsoil, current assessments often consider the topsoil only. Furthermore, mapping efforts are hampered by the limited spatial density of these topsoil measurements. The aim of this study was to assess the SOC stock in the upper 100cm of soil in 30,556ha of Low-Input High-Diversity systems, such as nature reserves, in Flanders (Belgium) and compare this estimate with the stock found in the topsoil (upper 15cm). To this end, we combined depth extrapolation of 139 measurements limited to the topsoil with four digital soil mapping techniques: multiple linear regression, boosted regression trees, artificial neural networks and least-squares support vector machines. Particular attention was given to vegetation characteristics as predictors. For both the stock in the upper 15cm and 100cm, a boosted regression trees approach was most informative as it resulted in the lowest cross-validation errors and provided insights in the relative importance of predictors. The predictors of the stock in the upper 100cm were soil type, groundwater level, clay fraction and community weighted mean (CWM) and variance (CWV) of plant height. These predictors, together with the CWM of specific leaf area, aboveground biomass production, CWV and CWM of rooting depth, terrain slope, CWM of mycorrhizal associations and species diversity also explained the topsoil stock. Our total stock estimates show that focusing on the topsoil (1.63Tg OC) only considers 36% of the stock in the upper 100cm (4.53Tg OC). Given the magnitude of subsoil OC and its dependency on typical ecosystem characteristics, it should not be neglected in regional ecosystem service assessments.
土壤有机碳(SOC)储量是生态系统服务评估的一个重要指标。尽管总储量的相当一部分储存在亚土层中,但当前的评估往往只考虑表土层。此外,由于这些表土测量的空间密度有限,测绘工作受到阻碍。本研究的目的是评估佛兰德斯(比利时)30556 公顷低投入高多样性系统(如自然保护区)上层 100cm 土壤中的 SOC 储量,并将这一估计与上层土壤(上层 15cm)中的储量进行比较。为此,我们将 139 个仅限于表土的测量值的深度外推与四种数字土壤制图技术相结合:多元线性回归、提升回归树、人工神经网络和最小二乘支持向量机。特别关注了植被特征作为预测因子。对于上层 15cm 和 100cm 的储量,提升回归树方法最具信息量,因为它导致了最低的交叉验证误差,并提供了关于预测因子相对重要性的见解。上层 100cm 储量的预测因子是土壤类型、地下水位、粘粒分数和群落加权均值(CWM)和方差(CWV)的植物高度。这些预测因子,加上比叶面积、地上生物量生产、根系深度的 CWV 和 CWM、地形坡度、菌根共生体和物种多样性的 CWM,也解释了表土储量。我们的总储量估计表明,只关注表土(1.63Tg OC)只考虑了上层 100cm 储量的 36%(4.53Tg OC)。鉴于亚土层 OC 的巨大规模及其对典型生态系统特征的依赖,在区域生态系统服务评估中不应忽视它。