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首页> 外文期刊>Quaternary International >Role of geomorphic surface on the above-ground biomass and soil organic carbon storage in a semi-arid region of Iranian loess plateau
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Role of geomorphic surface on the above-ground biomass and soil organic carbon storage in a semi-arid region of Iranian loess plateau

机译:地貌表面对伊朗黄土高原半干旱地区地上生物质和土壤有机碳储量的作用

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摘要

The so-called Iranian loess plateau is a unique landscape with a complex topography and steppe vegetation developed under semi-arid climate. We studied the relationships between geomorphic features, soils, biomass of above-ground vegetation (biomass) and soil organic carbon storage (SOCS) to further enhance our understanding of geomorphological processes, soil formation and evaluating SOCS in this strongly dissected landscape. Based on the previous knowledge, the effect of slope aspect on differentiation of soils is considerable in the studied area. Therefore, slope aspect was included as a phase of the geomorphic surface (PGS) in the geomorphic hierarchy to better analyze and understand the soil variation and development. A total of 220 soil samples were taken in different PGS from three depths 0-20, 20-40 and 40-60 cm. For additional details, biomass sampling was collected on 1 m(2) quadrat in every location where the soil samples were taken. Results showed that the 0-20 cm layer with 2.13 kg m(-2) had the maximum amount of SOC density (SOCD). Among studied units, moderately flat plain (VA111), loess tableland (TB111) and middle hill with north aspect (Hi211_2) had the highest SOCD compared to other units in the three studied depths. The results also indicated that PGS Hi211_2 had a significantly higher SOCD and biomass than PGS middle hill with south aspect (Hi211_1) in three soil layers. The highest values of SOCS were similarly found in the surface soil layer of PGS Hi211_2 accounting for 42816.55 Mg equal to 36.84% of total SOCS. In all PGSs, there were a positive significant correlations between biomass and SOCD (r(2) = 0.62, p = 0.01, n = 80). Therefore, the present study revealed that the variation of SOCD is mainly controlled by the PGS in hillslope landscape. Findings of SOCS denoted the importance of protecting surface and subsurface soil layers in hillslope to store SOC. In general, an accurate understanding of geomorphic surface is needed to accurately estimate SOCS, biomass and to evaluate soil and ecosystem related effects on global warming of ecologically sensitive semi-arid areas.
机译:所谓的伊朗黄土高原是一种独特的景观,具有复杂的地形和草原植被,在半干旱气候下开发。我们研究了地貌特征,土壤,地上植被(生物质)和土壤有机碳储存(SOC)之间的关系,以进一步增强我们对这种强烈解剖的景观中对地貌过程,土壤形成和评估SoC的理解。基于先前的知识,研究区坡度方面对土壤分化的影响是相当大的。因此,将斜率方面包含在地貌层次中的几何表面(PGS)的阶段,以更好地分析和理解土壤变异和发育。在不同的PGS中,来自三个深度0-20,20-40和40-60cm的不同pg,总共220个土壤样品。有关额外的细节,将生物质采样在1米(2)Quadrat上收集在拍摄土壤样品的每个位置。结果表明,含有2.13千克M(-2)的0-20厘米层具有最大的SOC密度(SOCD)。在学习的单位中,适度平平的平原(VA111),黄土大鼠(TB111)和北方方面的中山(HI211_2)与三个研究深度的其他单位相比,Socd的最高社会。结果还表明,PGS Hi211_2的SoCD和生物量明显高于PGS中山,其中三层土壤层中的南方面(Hi211_1)。 SOC的最高值类似地发现在PGS HI211_2的表面土壤层中,占42816.55mg等于总SOC的36.84%。在所有PGS中,生物质和SOCD(R(2)= 0.62,P = 0.01,N = 80)之间存在正显着的相关性。因此,本研究表明,SOCD的变化主要由山坡景观中的PGS控制。 SOC的结果表示保护山坡储存SOC的表面和地下土层的重要性。通常,需要准确地理解地貌表面,以准确估计SOC,生物质和评估土壤和生态系统对生态敏感半干旱地区的全球变暖的影响。

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