Department of Zoology, Oklahoma State University , Stillwater, Oklahoma 74078, United States.
Environ Sci Technol. 2014 Apr 15;48(8):4282-8. doi: 10.1021/es404883s. Epub 2014 Mar 31.
Watershed cultivation and subsequent soil erosion remains the greatest threat to the service provisioning of playa wetlands in the High Plains. The U.S. Department of Agriculture's (USDA) Conservation Reserve Program (CRP) plants perennial vegetation cover on cultivated lands including playa watersheds, and therefore, the program influences sediment deposition and accumulation in playas. Our objective was to measure the effects of the CRP on sediment deposition by comparing sediment depth and present/historic size characteristics in 258 playas among three High-Plains subregions (northern, central, and southern) and the three dominant watershed types: cropland, CRP, and native grassland. Sediment depth and resultant volume loss for CRP playas were 40% and 57% lower than cropland playas, but 68% and 76% greater than playas in native grassland. Playas in CRP had remaining volumes exceeding those of cropland playas. Grassland playas had nearly three times more original playa volume and 122% greater wetland area than CRP playas. Overall, playas were larger in the south than other subregions. Sediment depth was also three times greater in the south than the north, which resulted in southern playas losing twice as much total volume as northern playas. However, the larger southern playas provide more remaining volume per playa than those in other subregions. The results of this study demonstrate the importance of proper watershed management in preserving playa wetland ecosystem service provisioning in the High Plains. Furthermore, we identify regional differences in playas that may influence management decisions and provide valuable insight to conservation practitioners trying to maximize wetland services with limited resources.
流域开垦和随后的土壤侵蚀仍然是高平原干盐湖服务提供的最大威胁。美国农业部(USDA)的保护储备计划(CRP)在包括干盐湖流域在内的耕地上种植多年生植被,因此,该计划会影响干盐湖的泥沙沉积和堆积。我们的目标是通过比较三个高平原亚区(北部、中部和南部)和三种主要流域类型(耕地、CRP 和原生草地)的 258 个干盐湖的泥沙深度和当前/历史大小特征,来衡量 CRP 对泥沙沉积的影响。CRP 干盐湖的泥沙深度和由此产生的体积损失分别比耕地干盐湖低 40%和 57%,但比原生草地干盐湖高 68%和 76%。CRP 干盐湖的剩余体积超过了耕地干盐湖。草地干盐湖的原始干盐湖体积几乎是 CRP 干盐湖的三倍,湿地面积是 CRP 干盐湖的 122%。总体而言,南部干盐湖比其他亚区更大。泥沙深度在南部也比北部大三倍,这导致南部干盐湖的总体积损失是北部的两倍。然而,较大的南部干盐湖每个干盐湖的剩余体积都比其他亚区多。本研究结果表明,在高平原地区,适当的流域管理对于保护干盐湖湿地生态系统服务提供具有重要意义。此外,我们确定了干盐湖的区域差异,这可能会影响管理决策,并为试图在有限资源的情况下最大限度地发挥湿地服务的保护工作者提供宝贵的见解。