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首页> 外文期刊>Journal of Asian earth sciences >Stable and radioactive carbon in forest soils of Chhattisgarh, Central India: Implications for tropical soil carbon dynamics and stable carbon isotope evolution
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Stable and radioactive carbon in forest soils of Chhattisgarh, Central India: Implications for tropical soil carbon dynamics and stable carbon isotope evolution

机译:印度中部恰蒂斯加尔邦森林土壤中的稳定碳和放射性碳:对热带土壤碳动力学和稳定碳同位素演化的影响

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摘要

Soils from two sites viz. Kotumsar and Tirathgarh, located similar to 5 km apart in a tropical reserve forest (18 degrees 52'N, 81 degrees 56'E) in central India, have been explored for soil organic carbon (SOC) content, its mean residence time (MRT) and the evolution of stable carbon isotopic composition (delta C-13). SOC stocks in the upper 30 cm of soil layers are similar to 5.3 kg/m(2) and similar to 3.0 kg/m(2); in the upper 110 m are similar to 10.7 kg/m(2) and similar to 7.8 kg/m(2) at Kotumsar and Tirathgarh, respectively. SOC decreases with increasing depth. Bomb carbon signature is observed in the upper similar to 10 cm. Organic matters in the top soil layers (0-10 cm) have MRTs of the order of a century which increases gradually with depths, reaching 3500-5000 yrs at similar to 100 cm. delta C-13 values of SOC increase with depth, the carbon isotopic fractionation is obtained to be -1.2 parts per thousand and -3 parts per thousand for soils at Kotumsar and Tirathgarh, respectively, confirmed using Rayleigh isotopic fractionation model. The evolution of delta C-13 in soils was also studied using a modified Rayleigh fractionation model incorporating a continuous input into the reservoir: the depth profiles of delta C-13 for SOC show that the input organic matter from surface into the deeper soil layers is either insignificant or highly labile and decomposes quite fast in the top layers, thus making little contribution to the residual biomasses of the deeper layers. This is an attempt to understand the distillation processes that take place in SOC, assess the extent of decomposition by microbes and effect of percolation of fresh organic matter into dipper soil layers which are important for stable isotope based paleoclimate and paleovegetation reconstruction and understanding the dynamics of organic carbon in soils. (C) 2016 Elsevier Ltd. All rights reserved.
机译:来自两个地点的土壤。考察了位于印度中部热带储备森林(18度52'N,81度56'E)中相距约5公里的Kotumsar和Tirathgarh的土壤有机碳(SOC)含量,平均停留时间(MRT) )和稳定碳同位素组成的演化(δC-13)。土层上方30厘米的SOC储量类似于5.3 kg / m(2)和3.0 kg / m(2);在上部110 m处,分别在Kotumsar和Tirathgarh分别类似于10.7 kg / m(2)和7.8 kg / m(2)。 SOC随着深度的增加而降低。在上部大约10 cm处观察到炸弹碳签名。最高土壤层(0-10厘米)中的有机物具有大约一个世纪的MRT,并且随着深度的增加而逐渐增加,在接近100 cm时达到3500-5000年。 SOC的δC-13值随深度增加而增加,使用瑞利同位素分馏模型证实,对于Kotumsar和Tirathgarh的土壤,碳同位素分馏分别为-1.2千分率和-3千分之三。还使用修改后的瑞利分馏模型研究了土壤中δC-13的演化,该模型将连续输入纳入了储层:SOCδC-13的深度剖面表明,从地表到较深土壤层的输入有机物为无论是微不足道的还是高度不稳定的,并且在顶层的分解速度都非常快,因此对较深层的残留生物量几乎没有贡献。试图了解SOC中发生的蒸馏过程,评估微生物分解的程度以及新鲜有机物渗入北斗土壤层的作用,这对于稳定同位素基古气候和古植被的重建非常重要,并了解有机物的动力学。土壤中的有机碳。 (C)2016 Elsevier Ltd.保留所有权利。

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