基于柱研究的氯化物在不同土壤中传输参数的识别

IF 0.9 Q3 GEOLOGY
Geologos Pub Date : 2019-12-01 DOI:10.2478/logos-2019-0024
Damian Pietrzak, J. Kania, E. Kmiecik, Katarzyna Wątor
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引用次数: 4

摘要

摘要了解地下水中化学物质的运输模式对于评估其潜在影响至关重要。在本研究中,使用柱实验研究了注入三种不同土壤的氯化物示踪剂的流动性。柱试验是在稳态条件下进行的,以确定氯化物通过土壤迁移的参数。基于穿透曲线,使用CXTFIT/STANMOD软件计算了每个土壤样品的孔隙水速度、分散系数和分散常数。细砂的孔隙水速度范围为0.31 cm/min,粉砂为0.35 cm/min,细粒砂为0.40 cm/min。粉砂的分散系数和分散常数最高(分别为0.55 cm2/min和1.55 cm),而细砂的最小值(分别为0.059 cm2/min和0.19 cm)。氯化物(保守示踪剂)的柱实验是进一步研究的初步阶段,将进行进一步研究,以研究选定的新烟碱类化合物(反应示踪剂)在不同土壤中的迁移参数。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Identification of transport parameters of chlorides in different soils on the basis of column studies
Abstract Knowledge of transport patterns of chemicals in groundwater is essential for environmental assessment of their potential impact. In the present study, the mobility of a chloride tracer injected into three different soils was investigated, using column experiments. The column tests were performed under steady-state conditions to determine parameters of chloride migration through soils. Based on breakthrough curves, pore-water velocity, dispersion coefficient and dispersivity constant were calculated for each soil sample using CXTFIT/STANMOD software. Pore-water velocity was in the range of 0.31 cm/min for fine sand, to 0.35 cm/min for silty sand and to 0.40 cm/min for vari-grained sand. The highest values of dispersion coefficient and dispersivity constant were observed for silty sand (0.55 cm2/min and 1.55 cm, respectively), while the lowest value was found for fine sand (0.059 cm2/min and 0.19 cm, respectively). Column experiments for chlorides (conservative tracer) are a preliminary stage for further research which will be undertaken to investigate migration parameters of selected neonicotinoids (reactive tracers) through different soils.
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来源期刊
Geologos
Geologos GEOLOGY-
CiteScore
1.70
自引率
0.00%
发文量
7
审稿时长
12 weeks
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