孟加拉Arial Beel湿地土壤有机碳分异研究

Monera Akter Eva, Mahmudul Islam Piash, M. Hossain, Z. Parveen
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引用次数: 4

摘要

对孟加拉国基准湿地土壤(Arial Beel)垂直剖面的有机碳组分及其动态进行了研究,研究了有机碳组分对土壤、水和植物生物量生态系统生物地球化学的直接影响。Sara和Arial两个不同的土壤系列具有pH值、含水量、质地等级、CEC、有机碳(SOC)、容重和总有机质等特征。采用不同的萃取方法对水溶性组分(WSC)、热水可萃取组分(HWC)、水溶性组分(WSC)、水溶性组分(HWC)和水溶性组分(HWC)进行萃取。80℃),不稳定馏分(CaCl2-可萃取;LF),中等不稳定馏分(焦磷酸盐-可提取;MLF)、多芳馏分(甲苯+甲醇可萃取)、微生物生物量C馏分(MBF)和剩余抗性馏分(RF)。总有机碳含量为0.72 ~ 1.95%;地表C含量高于地下C含量,长时间淹水增加最多。土壤的高CEC与HWC、MBC和RF呈正相关。在大多数土壤中,表层和底层的DOC含量都高于地下层,尤其是MLF含量。HWC和ML分数非常显著(p为1%),对进一步退化具有相对的抗性,可能被认为是封存的C。短的淹没期和冬季Robi作物的范围可能导致Sara土壤的有机C和RF相对低于Arial。此外,Sara系列的DOC分数含量较低,且随深度的增加而减少,而Arial系列的DOC分数含量在剖面内变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fractionation of Organic Carbon in Arial Beel Wetland Soils of Bangladesh
A study was conducted to determine the organic carbon fractions in the vertical sections of a benchmark wetland soil of Bangladesh (Arial Beel) and their dynamics that directly affect the biogeochemistry of soil, water and plant biomass ecosystem. Two distinctive soil series viz. Sara and Arial are characterized such as pH, moisture content, textural class, CEC, organic carbon (SOC), bulk density and total organic matter etc. Different extraction methods were used for the fractionation of dissolved organic carbon such as water-soluble Fraction (WSC), hot water extractable fraction (HWC; 80°C), labile fraction (CaCl2- extractable; LF), moderately labile fraction (Pyrophosphate-extractable; MLF), polyaromatic fraction (toluene + methanol extractable), Microbial Biomass C Fraction (MBF) and the remaining Resistant Fraction (RF). The total organic carbon content ranges from 0.72 to 1.95%; surface horizons had higher C than underneath horizons and prolonged inundation increased the C content mostly. Higher CEC of the soils had a positive correlation to HWC, MBC and RF. The DOC content particularly MLF was found higher in surface and substratum than subsurface horizons in most of the soils. The HWC and ML fraction had highly significant (p 1%) which is relatively resistant to further degradation and might be considered as sequestered C. Short inundated period and scope of winter Robi crops might have caused Sara soil to have relatively lower organic C and RF than Arial. Moreover, the amount of DOC fractions in Sara series was lower and that decreased with depth but in Arial series, fractions varied within the profile.
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