加利纳斯河流域沉积物金属浓度作为生态系统恢复的指标

M. Hornberger, S. Murphy, Elizabeth Tomaszewski, J. Blake
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引用次数: 0

摘要

野火后影响和恢复的措施通常包括基于成分的方法,以确定自然和/或人为干扰。在评估与动员和运输有关的趋势方面,水质和河床沉积物研究就是两个这样的例子。2022年,Calf Canyon/Hermits Peak野火烧毁了加利纳斯河流域95%的地区。由于El Porvenir矿区(石英-伟晶岩矿脉)位于流域内,因此使用金属浓度来建立“火灾后条件”的基线,目的是评估空间和时间上的采收率。火灾发生5个月后收集了加利纳斯河和几条支流的河床沉积物样本。样品被筛选到<63µm,以减少粒度偏差,并允许相对于传统采矿活动的空间比较,并分析砷、镉和铜的浓度。在Gallinas Creek中,砷浓度在最上游的站点(Oak Flat的Gallinas Creek,为4.1±1.1µg/g)最低,在最下游的站点(Montezuma附近的Gallinas Creek,为5.3±0.3µg/g)最高。比弗溪子流域河流中的砷浓度比加利纳斯高出两倍,从6-10微克/克不等。镉浓度也有类似的规律:加利纳斯河上游站点的镉浓度最低(0.2±0.1µg/g),下游站点的镉浓度高3倍(0.6±0.2µg/g)。比弗溪和间歇溪流中的镉浓度变化很大,在0.4-0.7µg/g之间。与砷和镉不同,加利纳斯的铜没有单向的下游下降,除了Hermits Peak矿山坑道口附近的沉积物沉积物(100-443微克/克)外,所有地点的铜浓度都很低(14-25微克/克),可能是由于靠近传统的采矿活动。虽然非生物指标是确定金属来源的关键,但与金属浓度升高有关的生物效应只能推断。利用常驻水生生物进行组织残留研究,测量生物利用度,并提供化学暴露与生物效应之间的直接联系。底栖大型无脊椎动物没有出现在任何沉积物监测站,可能是由于野火造成的物理干扰(例如,高浊度、冲刷、泥石流)。然而,随着生境条件的改善,水生昆虫将重新定居,并作为本研究的一部分,允许进行组织金属分析和生态系统恢复的生物学评估。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Bed Sediment Metal Concentrations as Indicators of Ecosystem Recovery in the Gallinas Creek Watershed
Measures of post-wildfire effects and recovery often include constituent-based approaches that identify natural and/or anthropogenic disturbance. Water quality and bed sediment studies are two such examples in assessing trends associated with mobilization and transport. In 2022, the Calf Canyon/Hermits Peak Wildfire burned 95% of the Gallinas Creek watershed. Because the El Porvenir Mining District (Quartz-Pegmatite vein) lies within the watershed, metal concentrations were used to establish a baseline of “post-fire condition” with a goal of evaluating recovery over space and time. Bed sediment samples from Gallinas Creek and several tributaries were collected 5 months post fire. Samples were sieved to <63 µm to reduce grainsize bias and allow for spatial comparisons relative to legacy mining activities, and analyzed for arsenic, cadmium, and copper concentrations. In Gallinas Creek, arsenic concentrations were lowest at the most upstream station (Gallinas Creek at Oak Flat, 4.1 ± 1.1 µg/g) and greatest at the most downstream station (Gallinas Creek near Montezuma, 5.3 ± 0.3 µg/g). Arsenic concentrations in streams in the Beaver Creek sub-watershed were up to twofold higher than in the Gallinas, ranging from 6-10 µg/g. Cadmium concentrations followed a similar pattern: concentrations were lowest in the most upstream station on the Gallinas (0.2 ± 0.1 µg/g) and three-fold higher at the downstream station (0.6 ± 0.2 µg/g). Concentrations of cadmium in Beaver Creek, and intermittent streams, were variable, ranging from 0.4-0.7 µg/g. Unlike arsenic and cadmium, there was no unidirectional downstream decline of copper in the Gallinas, and concentrations were low (14-25 µg/g) at all sites apart from a sediment deposit near the mouth of the Hermits Peak Mine adit (100-443 µg/g), likely due to the proximity to legacy mining activities. Although abiotic indicators are key in identifying metal sources, biological effects associated with elevated metal concentrations can only be inferred. Tissue residue studies using resident aquatic organisms measure bioavailability and provide a direct link between chemical exposure and biological effects. Benthic macroinvertebrates were not present at any of the sediment monitoring stations, likely due to the physical disturbance (e.g., high turbidity, scour, debris flows) caused by the wildfire. However, as habitat conditions improve, aquatic insects will recolonize, and, as part of this study, allow for tissue metal analysis and biological assessment of ecosystem recovery.
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