Spatial analysis of borrow pits along the Platte River in south-central Nebraska, USA, in 1957 and 2016

N. Pauley, M. Harner, E. Buckley, P. Burger, Keith Geluso
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引用次数: 4

Abstract

: The Central Platte River Valley (CPRV) of Nebraska provides critical habitat for wildlife, while serving agricultural, indus trial, and other human uses. Mining of sand and gravel from the floodplain of the Platte River has supported construction of roads and other uses, and this extraction has created many borrow-pit ponds, lakes, and other small bodies of standing water (hereafter borrow-pits), further transforming riparian and prairie habitats. The objective of this study was to compare the abundance, size, and distribution of borrow pits before construction of Interstate 80 (1957) and at present (2016) from Lexington to Chapman, Nebraska, a length of river spanning about 146 km (90 mi) and sometimes referred to as the Big Bend Reach. Orthorectified aerial imagery of the Platte River was obtained for years 1957 and 2016, and we digitized the standing bodies of water within the floodplain in Arc -GIS. Total numbers of borrow pits and measures of pit shape were calculated and compared between floodplain regions where im agery overlapped. From 1957 to 2016, the number of borrow pits increased from 300 to 786, total area occupied by pits expanded by 538%, and total shoreline of pits increased by 261%. In 2016, aerial imagery was available for a larger extent of the floodplain and contained a total of 1,062 borrow pits covering 16 km 2 (6 mi 2 ), with a total shoreline of 581 km (361 mi). For context, the Platte River channels’ approximate area was 45 km 2 (17 mi 2 ) and shoreline 1,582 km (983 mi) between Lexington and Chapman, Nebraska, in 2016. Results provide insight into historical and current presence, distribution, and shape of borrow pits along the Platte River, as well as serve as a reference point for future studies investigating regional landscape change and ecological effects of creating hun dreds of borrow pits on the floodplain.
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1957年和2016年美国内布拉斯加州中南部普拉特河沿岸取土坑的空间分析
:内布拉斯加州的中央普拉特河谷(CPRV)为野生动物提供了重要的栖息地,同时为农业、工业和其他人类用途服务。从普拉特河泛滥平原开采沙子和砾石支持了道路建设和其他用途,这种开采创造了许多取土坑池塘、湖泊和其他小型积水(以下简称取土坑),进一步改变了河岸和草原栖息地。本研究的目的是比较80号州际公路建设之前(1957年)和现在(2016年)从列克星敦到内布拉斯加州查普曼的取土坑的丰度、大小和分布,这条河长约146公里(90英里),有时被称为大弯河段。普拉特河的正射校正航空图像是在1957年和2016年获得的,我们在Arc-GIS中对泛滥平原内的直立水体进行了数字化。计算并比较了河流重叠的洪泛平原地区的取土坑总数和坑形测量。从1957年到2016年,取土坑的数量从300个增加到786个,取土坑占用的总面积扩大了538%,取土坑总海岸线增加了261%。2016年,航空图像可用于更大范围的泛滥平原,共包含1062个取土坑,占地16平方公里(6英里),总海岸线为581公里(361英里)。就上下文而言,2016年,位于内布拉斯加州列克星敦和查普曼之间的普拉特河河道的大致面积为45平方公里(17英里),海岸线为1582公里(983英里)。研究结果深入了解了普拉特河沿岸取土坑的历史和现状、分布和形状,并为未来研究区域景观变化和在泛滥平原上建造大量取土坑的生态影响提供了参考。
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