Landuse and Physiographic Region Effects on Soil Carbon and Nitrogen Sequestration in Arkansas

Marya McKee, K. Brye, L. Wood
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引用次数: 1

Abstract

Increasing understanding of soil carbon (C) sequestration dynamics and general functioning in disappearing native grassland ecosystems, has the potential to enhance soil rehabilitation and ecosystem restoration. The objective of this study was to evaluate the effects of landuse (native tallgrass prairie and managed agriculture) and physiographic region (northwest Arkansas and east-central Arkansas) on the change in soil C and nitrogen (N) storage and other soil properties over a 15-year period. Despite the native prairie losing soil C at a rate of 4.7 Mg ha-1 year-1 over the 15-year duration of this study, soil C storage in 2016 was more than 2.5 times greater in the native prairie than in the cultivated agroecosystems in the Grand Prairie. Averaged across landuse, TC concentration (P
阿肯色州土地利用和地理区域对土壤碳氮固存的影响
增加对土壤碳(C)固存动态及其在消失的原生草地生态系统中的一般功能的了解,有可能加强土壤修复和生态系统恢复。本研究的目的是评估土地利用(原生高草草原和管理农业)和地理区域(阿肯色州西北部和阿肯色州中东部)在15年期间对土壤C和氮(N)储量及其他土壤性质变化的影响。尽管在本研究的15年期间,原生草原土壤C的流失速度为4.7 Mg ha-1 -1,但2016年,原生草原的土壤C储存量是大草原耕作农业生态系统的2.5倍以上。各土地利用类型的平均碳水化合物浓度(P
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