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温度对虹鳟鱼(Oncorhynchus mykiss)中从水力压裂返排液和产出水中菲积累的影响。

Effect of temperature on phenanthrene accumulation from hydraulic fracturing flowback and produced water in rainbow trout (Oncorhynchus mykiss).

机构信息

Department of Biological Sciences, University of Alberta, Edmonton, Alberta, Canada.

Department of Biological Sciences, University of Alberta, Edmonton, Alberta, Canada.

出版信息

Environ Pollut. 2021 Mar 1;272:116411. doi: 10.1016/j.envpol.2020.116411. Epub 2020 Dec 30.

Abstract

Hydraulic fracturing has become widely used in recent years to access vast global unconventional sources of oil and gas. This process involves the injection of proprietary mixtures of water and chemicals to fracture shale formations and extract the hydrocarbons trapped within. These injection fluids, along with minerals, hydrocarbons, and saline waters present within the formations being drilled into, return to the surface as flowback and produced water (FPW). FPW is a highly complex mixture, containing metals, salts and clay, as well as many organic chemicals, including polycyclic aromatic hydrocarbons such as phenanthrene. The present study sought to determine the effects of temperature on the accumulation of phenanthrene in rainbow trout (Oncorhynchus mykiss). This model organism resides in rivers overlapping the Montney and Duvernay formations, both highly developed formations for hydraulic fracturing. Rainbow trout acclimated to temperatures of 4, 13 and 17 °C were exposed to either 5% or 20% FPW, as well as saline mixtures representing the exact ionic content of FPW to determine the accumulation of radiolabelled C phenanthrene within the gill, gut, liver and gallbladder. FPW exposure reduced the overall accumulation of phenanthrene in a manner most often similar to high salinity exposure, indicating that the high ionic strength of FPW is the primary factor affecting accumulation. Accumulation was different at the temperature extremes (4 and 17 °C), although no consistent relationship was observed between temperature and accumulation across the observed tissues. These results indicate that several physiological responses occur as a result of FPW exposure and water temperature change which dictate phenanthrene uptake, particularly in the gills. Temperature (and seasonality) alone cannot be used to model the potential accumulation of polycyclic aromatic hydrocarbons after FPW spills.

摘要

水力压裂近年来在全球范围内得到了广泛应用,以获取大量的非常规石油和天然气资源。这一过程涉及注入专有配方的水和化学物质,以压裂页岩地层并提取被困在其中的碳氢化合物。这些注入流体与矿物质、碳氢化合物和正在钻探的地层中的盐水一起,作为回流和产出水(FPW)返回地面。FPW 是一种高度复杂的混合物,含有金属、盐和粘土,以及许多有机化学品,包括多环芳烃如菲。本研究旨在确定温度对虹鳟(Oncorhynchus mykiss)中菲积累的影响。这种模式生物生活在与 Montney 和 Duvernay 地层重叠的河流中,这两个地层都是水力压裂的高度发达地层。虹鳟适应 4、13 和 17°C 的温度,暴露于 5%或 20%的 FPW 以及代表 FPW 精确离子含量的盐水混合物中,以确定放射性标记的 C 菲在鳃、肠道、肝脏和胆囊中的积累。FPW 暴露以类似于高盐度暴露的方式降低了菲的总体积累,表明 FPW 的高离子强度是影响积累的主要因素。在温度极端(4 和 17°C)时积累情况有所不同,尽管在观察到的组织中没有观察到温度和积累之间的一致关系。这些结果表明,由于 FPW 暴露和水温变化,会发生几种生理反应,从而影响菲的吸收,特别是在鳃中。仅温度(和季节性)不能用于模拟 FPW 泄漏后多环芳烃的潜在积累。

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