Pierre Jon Paul, Abolt Charles J, Young Michael H
Energy and Earth Resources Program, Jackson School of Geosciences, The University of Texas at Austin, Austin, TX, USA.
Environ Manage. 2015 Jun;55(6):1262-75. doi: 10.1007/s00267-015-0492-2. Epub 2015 May 14.
We assess the spatial and geomorphic fragmentation from the recent Eagle Ford Shale play in La Salle County, Texas, USA. Wells and pipelines were overlaid onto base maps of land cover, soil properties, vegetation assemblages, and hydrologic units. Changes to continuity of different ecoregions and supporting landscapes were assessed using the Landscape Fragmentation Tool (a third-party ArcGIS extension) as quantified by land area and continuity of core landscape areas (i.e., those degraded by "edge effects"). Results show decreases in core areas (8.7%; 33,290 ha) and increases in landscape patches (0.2%; ~640 ha), edges (1.8%; ~6940 ha), and perforated areas (4.2%; ~16230 ha). Pipeline construction dominates landscape disturbance, followed by drilling and injection pads (85, 15, and 0.03% of disturbed area, respectively). An increased potential for soil loss is indicated, with 51% (5790 ha) of all disturbance regimes occurring on soils with low water-transmission rates (depth to impermeable layer less than 50 cm) and a high surface runoff potential (hydrologic soil group D). Additionally, 88% (~10,020 ha) of all disturbances occurred on soils with a wind erodibility index of approximately 19 kt/km(2)/year (0.19 kt/ha/year) or higher, resulting in an estimated potential of 2 million tons of soil loss per year. Results demonstrate that infrastructure placement is occurring on soils susceptible to erosion while reducing and splitting core areas potentially vital to ecosystem services.
我们评估了美国得克萨斯州拉萨尔县近期伊格福特页岩气田开发造成的空间和地貌破碎化情况。油井和管道被叠加在土地覆盖、土壤特性、植被群落和水文单元的底图上。使用景观破碎化工具(第三方ArcGIS扩展)评估了不同生态区域和支撑景观的连续性变化,该工具通过核心景观区域的土地面积和连续性(即那些受“边缘效应”退化的区域)进行量化。结果显示,核心区域减少了8.7%(约33290公顷),景观斑块增加了0.2%(约640公顷),边缘增加了1.8%(约6940公顷),穿孔区域增加了4.2%(约16230公顷)。管道建设主导了景观干扰,其次是钻井和注入平台(分别占受干扰区域的85%、15%和0.03%)。结果表明土壤流失的可能性增加,所有干扰区域中有51%(约5790公顷)发生在透水性低(不透水层深度小于50厘米)且地表径流潜力高(水文土壤组D)的土壤上。此外,所有干扰中有88%(约10020公顷)发生在风蚀性指数约为19节/千米²/年(0.19节/公顷/年)或更高的土壤上,导致每年估计有200万吨土壤流失。结果表明,基础设施建设正发生在易受侵蚀的土壤上,同时减少并分割了对生态系统服务可能至关重要的核心区域。