地下水位:对封闭填埋场nh4和CO 2排放的主要控制因素

A. Nwachukwu, N. Nwachukwu
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引用次数: 2

摘要

利用时间序列数据,确定了地下水位对封闭填埋场CH₄和CO₂浓度变化及其排放的影响。通过井内气体监测仪Gasclam(英国离子科学公司)收集了甲烷/二氧化碳浓度和环境参数的现场数据。采用线性回归分析确定地下气浓度与地下水位的相关性强弱。结果表明,在整个监测期内,CH₄和CO₂浓度与地下水位呈较强的负相关,各为0.5左右。考虑它们在地下水位上升和下降单期、地下水位上升单期和地下水位下降单期的浓度,R²略有提高;它们的相关性在95%的置信水平上显著增加。结果表明,地下水位波动是影响地下气体浓度排放和变化的主要驱动力,而不是气压和温度。这一发现进一步证实了先前的发现,即大气压力——被认为是污染地点CH₄和CO₂浓度变化/迁移的主要控制因素——并不总是如此。
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Water table: The dominant control on CH₄ and CO₂ emission from a closed landfill site
A time series dataset was conducted to ascertain the effect of water table on the variability in and emission of CH₄ and CO₂ concentrations at a closed landfill site. An in-situ data of methane/carbon dioxide concentrations and environmental parameters were collected by means of an in-borehole gas monitor, the Gasclam (Ion Science, UK). Linear regression analysis was used to determine the strength of the correlation between ground-gas concentration and water table. The result shows CH₄ and CO₂concentrations to be variable with strong negative correlations of approximately 0.5 each with water table over the entire monitoring period. The R² was slightly improved by considering their concentration over single periods of increasing and decreasing water table, single periods of increasing water table, and single periods of decreasing water table; their correlations increased significantly at 95% confidence level. The result revealed that fluctuations in groundwater level is the key driving force on the emission of and variability in ground-gas concentration and neither barometric pressure nor temperature. This finding further validates the earlier finding that atmospheric pressure – the acclaimed major control on the variability/migration of CH₄ and CO₂ concentrations on contaminated sites, is not always so.
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