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原油对非饱和带和饱和带中水分及示踪剂运移的影响。

Effects of crude oil on water and tracer movement in the unsaturated and saturated zones.

作者信息

Delin Geoffrey N, Herkelrath William N

机构信息

U.S. Geological Survey, Box 25046, MS 406, DFC, Denver, CO 80225, United States.

U.S. Geological Survey, 345 Middlefield Rd, MS496, Menlo Park, CA 94025, United States.

出版信息

J Contam Hydrol. 2017 May;200:49-59. doi: 10.1016/j.jconhyd.2017.03.007. Epub 2017 Mar 29.

Abstract

A tracer test was conducted to aid in the investigation of water movement and solute transport at a crude-oil spill site near Bemidji, Minnesota. Time of travel was measured using breakthrough curves for rhodamine WT and bromide tracers moving from the soil surface through oil-contaminated and oil-free unsaturated zones to the saturated zone. Results indicate that the rates of tracer movement were similar in the oil-free unsaturated and saturated zones compared to the oily zones. These results are somewhat surprising given the oil contamination in the unsaturated and saturated zones. Rhodamine tracer breakthrough in the unsaturated and saturated zones in general was delayed in comparison to bromide tracer breakthrough. Peak tracer concentrations for the lysimeters and wells in the oily zone were much greater than at the corresponding depths in the oil-free zone. Water and tracer movement in the oily zone was complicated by soil hydrophobicity and decreased oil saturations toward the periphery of the oil. Preferential flow resulted in reduced tracer interaction with the soil, adsorption, and dispersion and faster tracer movement in the oily zone than expected. Tracers were freely transported through the oily zone to the water table. Recharge calculations support the idea that the oil does not substantially affect recharge in the oily zone. This is an important result indicating that previous model-based assumptions of decreased recharge beneath the oil were incorrect. Results have important implications for modeling the fate and transport of dissolved contaminants at hydrocarbon spill sites.

摘要

在明尼苏达州贝米吉附近的一个原油泄漏场地,进行了一项示踪剂试验,以协助调查水的运动和溶质运移情况。利用若丹明WT和溴化物示踪剂的穿透曲线来测量运移时间,这些示踪剂从土壤表面穿过受油污染和未受油污染的非饱和带进入饱和带。结果表明,与含油带相比,在未受油污染的非饱和带和饱和带中,示踪剂的运移速率相似。考虑到非饱和带和饱和带中存在油污,这些结果有些出人意料。一般来说,与溴化物示踪剂的穿透相比,若丹明示踪剂在非饱和带和饱和带中的穿透有所延迟。含油带中渗漏计和井的示踪剂峰值浓度远高于未受油污染带相应深度处的浓度。土壤疏水性以及向油边缘方向油饱和度的降低,使得含油带中的水和示踪剂运移变得复杂。优先流导致示踪剂与土壤的相互作用、吸附和弥散减少,示踪剂在含油带中的运移速度比预期的要快。示踪剂可自由穿过含油带到达地下水位。补给量计算结果支持了油对含油带补给量没有实质性影响这一观点。这是一个重要结果,表明之前基于模型对油下方补给量减少的假设是错误的。这些结果对于模拟烃类泄漏场地中溶解污染物的归宿和运移具有重要意义。

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