尼日利亚伊莫州奥古塔湖二氧化碳排放与湿地土壤理化性质

A. W. Verla, J. Olumba, E. N. Verla
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引用次数: 1

摘要

湿地通过呼吸作用排放的二氧化碳约占世界二氧化碳排放量的5%,而这被认为是由土壤条件控制的。本研究的目的是建立沼泽土壤的理化参数与奥古塔湖1点CO2呼吸之间的联系。使用标准程序评估土壤参数,并将AZ 77535 CO2气体分析仪保持一臂距离以确定样品位置的CO2浓度。pH(5.03)、温度(28.16 oC)、电导率(108.56 uS/cm)、含水量(17.83%)和有机质的平均值分别为5.03、28.16、108.56、108.56和17.83(1.35%)。周平均[CO2]浓度(564 13.5 ~ 580.72.2 13.03 ppm)高于全球平均值(370 ppm)和湖周围所有地点,包括对照地点(425 2.5 ~ 438.2 2.0 ppm)。[CO2]与R2分别为(0.262)、(0.370)、(0.304)、(0.294)和(0.056),呈正相关。这表明CO2呼吸受土壤特性的调节。土壤特征的增加与二氧化碳浓度的增加相对应。这些发现有助于我们理解如何调整土壤特征以减少土壤呼吸的二氧化碳,从而减少湿地对全球变暖的贡献。
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Carbon dioxide emissions and wetland soil physicochemical properties in Oguta Lake, Imo State, Nigeria
Wetlands contribute around 5 percent of the world's carbon dioxide (CO2) emissions via respiration, which is believed to be controlled by soil conditions. The objective of this study is to establish a link between the physicochemical parameters of marsh soil and CO2 respiration at Oguta lake point one. Standard procedures were used to assess the soil parameters, and an AZ 77535 CO2 gas analyzer was held at arm's length to determine the CO2 concentration at the sample location. The mean values for pH (5.03), temperature (28.16 oC), electrical conductivity (108.56 uS/cm), moisture content (17.83 percent), and organic matter were 5.03, 28.16, 108.56, 108.56, and 17.83, respectively (1.35 percent). The mean weekly [CO2] concentrations (564 13.5 to 580.72.2 13.03 ppm) were greater than the global average (370 ppm) and all locations surrounding the lake, including the control site (425 2.5 to 438.2 2.0 ppm). Positive relationships were identified between [CO2] and R2 values of (0.262), (0.370), (0.304), (0.294), and (0.056), respectively. This demonstrates that CO2 respiration is regulated by soil characteristics. A rise in soil characteristics corresponded to an increase in CO2 concentration. These findings contribute to our understanding of how soil characteristics might be adjusted to reduce soil respired CO2 and, consequently, wetland contributions to global warming.
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