印度本地治里两个主要湿地沉积物碳储量

A. Miria, A. Khan
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引用次数: 1

摘要

研究的目的是评估Oussudu和Kaliveli沉积物中的碳储存模式,这两个湿地被认为是RAMSAR公约下的潜在保护湿地,并被政府宣布为鸟类保护区。分析了“地表水”中溶解氧和CO2的扩散速率,提出了沉积物碳储量与水体中氧/二氧化碳的关系。研究期间(2009 - 2011年)乌苏都和卡利韦里的溶解氧平均含量分别为17.28±3.25 mg/l和35.5±7.23 mg/l。Kaliveli的CO2扩散速率(13.31±2.71 mg/l)高于Oussudu(6.48±1.21 mg/l)。高水平的二氧化碳扩散导致酸化形成碳酸,这可能是Kaliveli沉积物钙含量高的原因。乌苏都沉积物的平均碳酸钙和有机质含量分别为2.11±0.51%和1.51±0.59%,卡利维利沉积物的平均碳酸钙和有机质含量分别为36.21±4.51%和0.46±0.16%。总有机碳含量为0.87±0.34%,总磷含量为27.38±0.56 (mg/L),总有机碳含量为0.27±0.09%,总磷含量为4.13±0.67 (mg/L)。沉积物中碳酸钙与有机质呈显著的反比关系,有机质与磷酸盐呈强烈的正相关关系。研究表明,乌苏都湖的碳主要通过有机质储存,卡利维利湖的碳主要通过碳酸钙储存。
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Sediment Carbon Storage of Two Main Wetlands in Pondicherry, India
Assessing the carbon storage patterns in the sediments of Oussudu and Kaliveli, considered as potential wetlands for conservation under RAMSAR convention and declared bird sanctuaries by the government was the objective of the study. Dissolved oxygen and CO2 diffusion rates in the 'surface waters' was analyzed and the relationship between the sediment carbon storage and oxygen/carbon dioxide in the waters was presented. The mean dissolved oxygen content for the study period (2009 - 2011) was 17.28 ± 3.25 mg/l for Oussudu and 35.5 ± 7.23 mg/l for Kaliveli respectively. The rate of CO2 diffusion was high (13.31±2.71 mg/l) in Kaliveli than in Oussudu (6.48±1.21 mg/l). High level of CO2 diffusion causes acidification forming carbonic acids which might be the cause of high levels of sediment calcium in Kaliveli. The mean calcium carbonate and organic matter content of sediment was 2.11±0.51% and 1.51±0.59% for Oussudu and 36.21±4.51% and 0.46±0.16% for Kaliveli respectively. The total organic carbon and phosphate content were 0.87±0.34% and 27.38±0.56 (mg/L) for Oussudu and 0.27±0.09% and 4.13±0.67 (mg/L) for Kaliveli respectively. There existed a significant inversely proportional relationship between calcium carbonate and organic matter and a strong positive relationship between organic matter and phosphate in the sediments. Our study reveals that majority of the carbon storage is through organic matter in Oussudu lake and through calcium carbonate in Kaliveli.
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