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Naproxen adsorption-desorption in a sandy aquifer matrix: characterisation of hysteretic behavior at two different temperature values.

机译:萘普生在含砂含水层基质中的吸附-解吸:表征两个不同温度值下的滞后行为。

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Adsorption/desorption processes (sorption isotherms) of Naproxen in a sandy aquifer matrix sediment were investigated using batch tests to compare Naproxen sorption behavior at 15 degrees C and 25 degrees C. Both temperatures are representative of the aquifer media and environmental conditions. Adsorption was well described by linear isotherms with low sorption affinity to aquifer material (Kd of 0.4 micro g kg-1) at both temperatures (15 degrees C and 25 degrees C). Desorption isotherm coefficients at 15 degrees C and 25 degrees C were 5.0 and 4.9, respectively. Naproxen hysteresis indices were between 9.98 and 10.8, indicating that a Naproxen fraction may be irreversibly fixed in the aquifer media, being higher at 25 degrees C (10.88) compared to 15 degrees C, showing a decreasing trend with increasing compound concentration at 15 degrees C. The low sorption of Naproxen leads to potential leaching to groundwater if present in irrigation water, and its prevalence in an aquifer media when directly injected in wells for groundwater recharge.
机译:使用分批测试研究了萘普生在砂质含水层基质沉积物中的吸附/解吸过程(吸附等温线),以比较萘普生在15摄氏度和25摄氏度下的吸附行为。两种温度均代表含水层介质和环境条件。在两个温度(15摄氏度和25摄氏度)下,对含水层材料(K d 为0.4 micro g kg -1 )的吸附亲和力低的线性等温线很好地描述了吸附)。 15摄氏度和25摄氏度的解吸等温系数分别为5.0和4.9。萘普生的磁滞指数在9.98到10.8之间,表明萘普生组分可能不可逆地固定在含水层介质中,在25摄氏度(10.88)时高于15摄氏度,随着15摄氏度化合物浓度的增加呈下降趋势。萘普生的低吸附率会导致潜在的沥滤(如果存在于灌溉水中),而直接注入井中以补充地下水时,其在含水层介质中的普遍性。

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