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首页> 外文期刊>Soil Science Society of America Journal >Soil-Specific Inventories of Landscape Carbon and Nitrogen Stocks under No-Till and Native Vegetation to Estimate Carbon Offset in a Subtropical Ecosystem
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Soil-Specific Inventories of Landscape Carbon and Nitrogen Stocks under No-Till and Native Vegetation to Estimate Carbon Offset in a Subtropical Ecosystem

机译:免耕和原生植被下土壤碳氮储量的土壤比重清单,估计亚热带生态系统的碳补偿

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摘要

Inventories of C and N footprints on a landscape scale are essential tools for estimating C offsets from agricultural emissions. Therefore, the aims of this study conducted in the subtropical humid ecosystem in southern Brazil were to: (i) conduct a soil-specific inventory of landscape soil C and N stocks with reference to soil order, soil texture, and land use/management type; (ii) estimate accretion rates for soil organic C (SOC) and total N (TN) for areas managed under no-till (NT) practices management with reference to native vegetation (NV) based on this inventory; (iii) generate a map of C stocks for each land use system; and (iv) calculate estimated C offset for the region through the use of NT compared to conventional tillage (CT). Soil samples were collected at 324 points to a 1-m depth from the entire region. Soil texture and duration of NT had a strong influence on C and N stocks. The average soil C stock across all types of soils for depths of 0-40 and 40-100 cm was 57.0 and 43.0%, respectively. The extrapolation of C stored in the 0- to 40-cm depth based on the NT management for 11 and 20 yr for 1.52 million hectare (Mha) was 9.08 +/- 0.62 Tg (1 Tg = 10(12) g) representing 11.9% of the C stored in all soil orders. The long-term of C sink capacity by conversion of arable land from CT to NT in this region is 33.2 Tg of CO2, with the C offset of 22.5% of all anthropogenic emissions.
机译:景观规模上的碳和氮足迹清单是估算农业排放中碳补偿的重要工具。因此,在巴西南部亚热带湿润生态系统中进行的这项研究的目的是:(i)参照土壤顺序,土壤质地和土地利用/管理类型,针对特定土壤进行景观土壤碳和氮储量清查。 ; (ii)根据此清单估算免耕(NT)措施管理下的土壤有机碳(SOC)和总氮(TN)的增生率,并参考原生植被(NV); (iii)生成每个土地使用系统的碳库图; (iv)与传统耕作(CT)相比,通过使用NT计算该区域的估算C偏移量。从整个区域以1-2点的深度采集324个土壤样品。土壤质地和NT持续时间对碳和氮储量有很大影响。 0-40和40-100 cm深度下,所有类型土壤的平均土壤碳储量分别为57.0%和43.0%。基于NT管理11年和20年1.52百万公顷(Mha),存储在0至40厘米深度的C的外推值为9.08 +/- 0.62 Tg(1 Tg = 10(12)g),代表11.9存储在所有土壤顺序中的碳的百分比。通过将耕地从CT转换为NT的长期碳吸收能力是33.2 Tg CO2,碳抵消了所有人为排放量的22.5%。

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