首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Estimating Soil Organic Carbon Density in the Otindag Sandy Land, Inner Mongolia, China, for modelling spatiotemporal variations and evaluating the influences of human activities
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Estimating Soil Organic Carbon Density in the Otindag Sandy Land, Inner Mongolia, China, for modelling spatiotemporal variations and evaluating the influences of human activities

机译:估算中国内蒙古奥特南地板砂土土壤有机碳密度,用于造型时空变化和评价人类活动影响

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Accurate quantitative estimates of Soil Organic Carbon Density (SOCD) can effectively represent regional carbon cycle processes and regulation mechanisms, and can serve as reference data when making land management decisions. Limited research, however, has been carried out in arid or desert zones covered with sparse vegetation, despite the fact that these cover wide areas of the earth and play a significant role in global carbon cycles. In this study, the Otindag Sandy Land and its surroundings (OSLAIS) in the Inner Mongolia Autonomous Region of China was selected as the study area. The study introduces a useful technique for making high spatial coverage SOCD estimates for drylands by utilizing GF-1 WFV optical satellite images and a time series of MODIS satellite remote sensing datasets, and using these to optimize parameters for simulation models in conjunction with other technical procedures that are described. The results showed that the resulting model's accuracy was 77.87%, R-2 = 0.8627, and so the SOCD estimates modelled by soil basal respiration (SBR) could be used for SOCD estimation and for analyzing the spatial distribution patterns across the OSLAIS. The average SOCD was 1.22 kgC/m(2) for the whole of the OSLAIS, and it had a heterogenous distribution pattern. The SOCD was closely related to the way the land was used in each area, and the average SOCD for the main land use types were: forest land = 2.88 kgC/m(2), farmland = 1.63 kgC/m(2), shrub land = 1.41 kgC/m(2), and grassland = 1.08 kgC/m(2). In conclusion, we believe that the proposed method, based on high-resolution GF-1 WFV data and optimized estimation models constructed by integrating climate and vegetation characteristic data, can effectively describe the spatial distribution patterns of SOC and SOCD in the OSLAIS area, in depth and in detail, especially for the areas where the SOCD values are high. We expect this research to provide useful technical support and scientific reference data for land management and for land degradation/desertification assessments, for the study area monitored, as well as across the whole dryland area of China.
机译:准确的土壤有机碳密度(SOCD)的定量估计可以有效地代表区域碳循环过程和调节机制,并可作为在制定土地管理决策时作为参考数据。然而,有限的研究已经在覆盖着稀疏植被的干旱或沙漠区域中进行的,尽管这些覆盖了地球的广泛区域,并且在全球碳循环中发挥着重要作用。在本研究中,选择了中国内蒙古自治区的奥特林格桑迪土地及其周围环境(Oslais)被选为研究区。该研究通过利用GF-1 WFV光学卫星图像和MODIS卫星遥感数据集的时间序列来介绍一种用于使旱地的高空间覆盖SOCD估计的有用技术,并使用这些来优化与其他技术过程的仿真模型参数那描述了。结果表明,所得的模型的准确性为77.87%,R-2 = 0.8627,因此由土壤基础呼吸(SBR)建模的SOCD估计可用于SoCD估计,并用于分析奥斯氏的空间分布图案。整个SOCD为整个OSLAI为1.22 kgc / m(2),它具有异质分布模式。 SoCD与土地在每个地区使用的方式密切相关,以及主要土地使用类型的平均SOCD是:林地= 2.88 kgc / m(2),农田= 1.63 kgc / m(2),灌木LAND = 1.41 kgc / m(2),草地= 1.08 kgc / m(2)。总之,我们认为,基于高分辨率GF-1 WFV数据和通过整合气候和植被特征数据构建的优化估计模型的方法可以有效地描述SOC和SOCD在Oslais地区的空间分布模式深度和详细,特别是对于SoCD值高的区域。我们预计这项研究可以为土地管理和土地退化/荒漠化评估提供有用的技术支持和科学参考数据,用于监测的研究区,以及整个中国整个旱地地区。

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