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Natural vegetation restoration is more beneficial to soil surface organic and inorganic carbon sequestration than tree plantation on the Loess Plateau of China

机译:黄土高原地区天然植被的恢复比树木人工林更有利于土壤表面有机碳和无机碳的固存

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摘要

Natural vegetation restoration and tree plantation are the two most important measures for ecosystem restoration on the Loess Plateau of China. However, few studies have compared the effects of the two contrasting measures on soil organic and inorganic carbon (SOC and SIC) sequestration or have further used SOC and SIC isotopes to analyze the inherent sequestration mechanism. This study examined a pair of neighboring small watersheds with similar topographical and geological backgrounds. Since 1954, natural vegetation restoration has been conducted in one of these watersheds, and tree plantation has been conducted in the other. The two watersheds have now formed completely different landscapes (naturally restored grassland and artificial forestland). Differences in soil bulk density, SOC and SIC content and storage, and SOC and SIC delta C-13 values were investigated in the two ecosystems in the upper 1 m of the soil. We found that SOC storage was higher in the grassland than in the forestland, with a difference of 14.90 Mg ha(-1). The vertical changes in the delta C-13(SOC) value demonstrated that the two ecosystems have different mechanisms of soil surface organic carbon accumulation. The SIC storage in the grassland was lower than that in the forestland, with a difference of 38.99 Mg ha(-1). The delta C-13(SIC) values indicated that the grassland generates more secondary carbonate than the forestland and that SIC was most likely transported to the rivers from the grassland as dissolved inorganic carbon (DIC). The biogeochemical characteristics of the grassland were favorable for the formation of bicarbonate. Thus, more DIC derived from the dissolution of root and microbial respired CO2 into soil water could have been transported to the rivers through flood runoff. It is necessary to study further the transportation of DIC from the grassland because this process can produce a large potential carbon sink. (C) 2014 The Authors. Published by Elsevier B.V.
机译:恢复自然植被和植树造林是黄土高原生态系统恢复的两个最重要措施。但是,很少有研究比较这两种对比措施对土壤有机碳和无机碳(SOC和SIC)固存的影响,或进一步使用SOC和SIC同位素分析内在固存机理。这项研究检查了一对具有相似地形和地质背景的相邻小流域。自1954年以来,在其中一个流域进行了自然植被恢复,在另一个流域进行了人工林。这两个流域现已形成完全不同的景观(自然恢复的草地和人工林地)。在土壤上部1 m的两个生态系统中,研究了土壤容重,SOC和SIC含量和存储以及SOC和SICδC-13值的差异。我们发现,草地上的SOC储存量比林地中的高,差异为14.90 Mg ha(-1)。 δC-13(SOC)值的垂直变化表明这两个生态系统具有不同的土壤表面有机碳积累机制。草原的SIC储存量比林地的SIC储存量低,相差38.99 Mg ha(-1)。 δC-13(SIC)值表明,草地产生的次生碳酸盐比林地多,并且SIC最有可能以草地中的溶解性无机碳(DIC)形式运到河流。草原的生物地球化学特征有利于碳酸氢盐的形成。因此,更多的由根和微生物呼吸的CO2溶解到土壤水中而产生的DIC可以通过洪水径流被输送到河流中。有必要进一步研究DIC从草原的运输,因为该过程会产生大量的潜在碳汇。 (C)2014作者。由Elsevier B.V.发布

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