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DOI: 10.1371/journal.pone.0084988
论文题名:
Soil Aggregates and Associated Organic Matter under Conventional Tillage, No-Tillage, and Forest Succession after Three Decades
作者: Scott Devine; Daniel Markewitz; Paul Hendrix; David Coleman
刊名: PLOS ONE
ISSN: 1932-6203
出版年: 2014
发表日期: 2014-1-20
卷: 9, 期:1
语种: 英语
英文关键词: Land use ; Agricultural soil science ; Particulates ; Physical geography ; Cereal crops ; Agriculture ; Forests ; Fractionation
英文摘要: Impacts of land use on soil organic C (SOC) are of interest relative to SOC sequestration and soil sustainability. The role of aggregate stability in SOC storage under contrasting land uses has been of particular interest relative to conventional tillage (CT) and no-till (NT) agriculture. This study compares soil structure and SOC fractions at the 30-yr-old Horseshoe Bend Agroecosystem Experiment (HSB). This research is unique in comparing NT and CT with adjacent land concurrently undergoing forest succession (FS) and in sampling to depths (15–28 cm) previously not studied at HSB. A soil moving experiment (SME) was also undertaken to monitor 1-yr changes in SOC and aggregation. After 30 years, enhanced aggregate stability under NT compared to CT was limited to a depth of 5 cm, while enhanced aggregate stability under FS compared to CT occurred to a depth of 28 cm and FS exceeded NT from 5–28 cm. Increases in SOC concentrations generally followed the increases in stability, except that no differences in SOC concentration were observed from 15–28 cm despite greater aggregate stability. Land use differences in SOC were explained equally by differences in particulate organic carbon (POC) and in silt-clay associated fine C. Enhanced structural stability of the SME soil was observed under FS and was linked to an increase of 1 Mg SOC ha−1 in 0–5 cm, of which 90% could be attributed to a POC increase. The crushing of macroaggregates in the SME soil also induced a 10% reduction in SOC over 1 yr that occurred under all three land uses from 5–15 cm. The majority of this loss was in the fine C fraction. NT and FS ecosystems had greater aggregation and carbon storage at the soil surface but only FS increased aggregation below the surface, although in the absence of increased carbon storage.
URL: http://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0084988&type=printable
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/19711
Appears in Collections:过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响

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作者单位: Warnell School of Forestry and Natural Resources, The University of Georgia, Athens, Georgia, United States of America;Warnell School of Forestry and Natural Resources, The University of Georgia, Athens, Georgia, United States of America;Odum School of Ecology, The University of Georgia, Athens, Georgia, United States of America;Odum School of Ecology, The University of Georgia, Athens, Georgia, United States of America

Recommended Citation:
Scott Devine,Daniel Markewitz,Paul Hendrix,et al. Soil Aggregates and Associated Organic Matter under Conventional Tillage, No-Tillage, and Forest Succession after Three Decades[J]. PLOS ONE,2014-01-01,9(1)
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