2018
DOI: 10.1016/j.geoderma.2018.03.032
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Spatial distribution of soil organic carbon in the ecologically fragile Horqin Grassland of northeastern China

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Cited by 37 publications
(24 citation statements)
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“…The study area covered 12% of the land area in the Loess Plateau, but the accumulation of stored SOC predicted by the IDW (ca 25.65 Tg) and OK (ca 25.86 Tg) methods accounted for only approximately 0.54% of the total SOC storage in the 0-100 cm layers in the Loess Plateau [60], indicating that both interpolation methods were suitable to estimate the storage of SOC and that the study area had considerable potential for carbon sequestration. In our study, approximately 70% of the SOC was stored in the 0-60 cm soil layers, which was consistent with a study conducted in the Horqin Grassland of northern China [28]. Furthermore, topography can indirectly affect SOC content by changing temperature and precipitation patterns [47,59], which may result in the overestimation or underestimation of SOC storage in the southern hills and gullies area with low sampling density.…”
Section: Estimation Of Soc Storagesupporting
confidence: 91%
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“…The study area covered 12% of the land area in the Loess Plateau, but the accumulation of stored SOC predicted by the IDW (ca 25.65 Tg) and OK (ca 25.86 Tg) methods accounted for only approximately 0.54% of the total SOC storage in the 0-100 cm layers in the Loess Plateau [60], indicating that both interpolation methods were suitable to estimate the storage of SOC and that the study area had considerable potential for carbon sequestration. In our study, approximately 70% of the SOC was stored in the 0-60 cm soil layers, which was consistent with a study conducted in the Horqin Grassland of northern China [28]. Furthermore, topography can indirectly affect SOC content by changing temperature and precipitation patterns [47,59], which may result in the overestimation or underestimation of SOC storage in the southern hills and gullies area with low sampling density.…”
Section: Estimation Of Soc Storagesupporting
confidence: 91%
“…Furthermore, topography can indirectly affect SOC content by changing temperature and precipitation patterns [47,59], which may result in the overestimation or underestimation of SOC storage in the southern hills and gullies area with low sampling density. Considering the high organic carbon content and its sensitivity to climate change and human disturbance in surface soils [28,40,60], we should allocate more sampling sites in the 0-60 cm soil layers while appropriately reducing sampling sites in the other soil layers, thus improving the estimation accuracy of SOC in similar ecosystems with relatively little funding and human resources.…”
Section: Estimation Of Soc Storagementioning
confidence: 99%
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“…on the south slope of the mountain. The temperature decreases and the precipitation increases with increasing altitude in this area ( Jin et al, 2017 ; Li et al, 2018 ). According to the vegetation investigation, the grassland was classified as alpine meadows at elevations of 3,350 m, 3,460 m, and 3 570 m and alpine shrub meadows at elevations of 3,680 m and 3,800 m.…”
Section: Methodsmentioning
confidence: 99%
“…The first one was that, unlike the sandblasting theory used in the other two schemes, the KOK scheme was built on the foundation of fragmentation theory, which was depicted as dust aggregates fragmented by saltators into smaller particles and vertically emitted to the atmosphere [44]. This might be not applicable in a region with large areas of grassland, shrub land, and cropland enriching organic matter [53], which are different from desert and barren land. The second might be ascribed to the dust emission coefficient C d that scaled the dust emission flux in a way which was similar (but not identical) to the dust source functions.…”
Section: Discussionmentioning
confidence: 99%