基于无人机高分辨率遥感的温带泥炭地泥炭土厚度和碳储存控制因素

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE
Yanfei Li , Maud Henrion , Angus Moore , Sébastien Lambot , Sophie Opfergelt , Veerle Vanacker , François Jonard , Kristof Van Oost
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引用次数: 0

摘要

泥炭地储存了大量的碳。然而,泥炭地是一个复杂的生态系统,即使在较小的尺度上,要可靠地估算出地球表面下储存了多少碳也是一项固有的挑战。在此,我们旨在建立控制土壤碳状况的地上和地下因素之间的联系,确定与碳储存相关的关键环境变量,并探索使用无人飞行器(UAV)遥感技术绘制泥炭地空间地图的潜力。我们将配备有红绿蓝(RGB)、多光谱、热红外和光探测与测距(LiDAR)传感器的无人机与地面穿透雷达(GPR)技术和传统的实地勘测相结合,对比利时上法涅斯地区的泥炭地山坡-洪泛平原景观进行了全面的三维测绘。我们的研究结果表明,泥炭厚度和土壤有机碳(SOC)储量(顶部 1 米)在空间上是异质的,地表地形对泥炭厚度和 SOC 储量的影响从微观到宏观尺度各不相同。泥炭厚度受宏观地形(= 0.46)的控制比 SOC 储量更强,而 SOC 储量受微观地形(= 0.21)的影响更大。当前植被对解释其空间变化的预测力很小。此外,无人机数据还提供了泥炭厚度和 SOC 储量的精确估算值,泥炭厚度的均方根误差为 0.16 米,SOC 储量的均方根误差为 59.25 吨/公顷,SOC 储量的均方根误差为 0.85。不过,仅使用激光雷达传感器的地形数据(泥炭厚度)和泥炭厚度与地形的组合(SOC 储量)作为预测变量,也能达到类似的效果。我们的研究填补了地表观测数据与地下隐藏碳库之间的空白。这不仅提高了我们评估 SOC 储量空间分布的能力,还有助于我们了解与这些高度异质性地貌中 SOC 储量相关的环境因素,为环境科学和气候预测提供启示。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Factors controlling peat soil thickness and carbon storage in temperate peatlands based on UAV high-resolution remote sensing

Peatlands store a large amount of carbon. However, peatlands are complex ecosystems, and acquiring reliable estimates of how much carbon is stored underneath the Earth’s surface is inherently challenging, even at small scales. Here, we aim to establish links between the above- and below-ground factors that control soil carbon status, identify the key environmental variables associated with carbon storage, as well as to explore the potential for using Unmanned Aerial Vehicle (UAV) remote sensing for spatial mapping of peatlands. We combine UAVs equipped with Red-Green-Blue (RGB), multispectral, thermal infrared, and light detection and ranging (LiDAR) sensors with ground-penetrating radar (GPR) technology and traditional field surveys to provide a comprehensive, 3-dimensional mapping of a peatland hillslope-floodplain landscape in the Belgian Hautes Fagnes. Our results indicate that both peat thickness and soil organic carbon (SOC) stock (top 1 m) are spatially heterogeneous and that the contributions from the surface topography to peat thickness and SOC stock varied from micro- to macro-scales. Peat thickness was more strongly controlled by macro-topography (R2 = 0.46) than SOC stock, which was more influenced by micro-topography (R2 = 0.21). Current vegetation had little predictive power for explaining their spatial variability. Additionally, the UAV data provided accurate estimates of both peat thickness and SOC stock, with RMSE and R2 values of 0.16 m and 0.85 for the peat thickness, and 59.25 t/ha and 0.85 for the SOC stock. However, similar performance can already be achieved by using only topographical data from the LiDAR sensor (for peat thickness) and a combination of peat thickness and topography (for SOC stock) as predictor variables. Our study bridges the gap between surface observations and the hidden carbon reservoir below. This not only allows us to improve our ability to assess the spatial distribution of SOC stocks, but also contributes to our understanding of the environmental factors associated with SOC storage in these highly heterogeneous landscapes, providing insights for environmental science and climate projections.

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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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