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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Changes in water stable aggregate and soil carbon accumulation in a no-tillage with weed mulch management site after conversion from conventional management practices.
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Changes in water stable aggregate and soil carbon accumulation in a no-tillage with weed mulch management site after conversion from conventional management practices.

机译:从常规管理方法转换后的免耕杂草覆盖管理场所的水稳定总量和土壤碳积累的变化。

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Soil carbon (C) is crucial for maintaining soil functions, and it increases after conversion of an agricultural field from conventional tillage management to no-tillage management due to decreasing human-induced soil disturbance and the modification of soil structure through ecosystem engineers such as earthworms. To improve soils and prevent degradation, understanding the effects of no-tillage management over time in changing water stable aggregates (WSA) and soil C is important. We investigated the changes in WSA and soil C at a site in Akame, Mie, Japan, operating a no-tillage with weed mulch management (NWM) system over a chronosequence from 0 to 17 years after conversion from conventional tillage practices (NWM for 0, 5, 10, 15, and 17 years). We measured weed aboveground biomass, litter accumulation, and root and earthworm density and biomass, and analyzed the WSA and C of bulk soil and each WSA size fraction. Weed aboveground biomass increased with site age, while litter accumulation, root biomass (soil depth of 0-4 cm), and earthworm density and biomass did not appear to be related to site age. Endogeic earthworm density and biomass tended to increase at year 5 of NWM compared to year 0. The WSA > 2 mm and soil C stock in WSA of > 2 mm increased over time under NWM at a soil depth of 0-15 cm, while the soil C stock of 0.25-1-mm WSA decreased at soil depths of 0-5 cm. The total soil C accumulation rate was 60 g C m-2 yr-1 at a soil depth of 0-25 cm over the NWM chronosequence. Therefore, our results indicated that by adopting NWM, C inputs to the soil from weed aboveground biomass, as well as increases in the WSA of > 2 mm, might be responsible for soil C sequestration.
机译:土壤碳(C)对于维持土壤功能至关重要,由于减少了人为的土壤干扰并通过生态系统工程师(例如the)对土壤结构进行了改造,因此从常规耕作管理向免耕管理转化后,土壤碳(C)会增加。为了改良土壤并防止土壤退化,了解随着时间推移免耕管理对改变水稳性团聚体(WSA)和土壤C的影响非常重要。我们调查了日本三重县赤濑市某地的WSA和土壤C的变化,该系统在从传统耕作方式转换后的0到17年的时间序列内使用杂草覆盖管理(NWM)系统进行了免耕(NWM为0 ,5、10、15和17岁)。我们测量了地上杂草的生物量,凋落物的积累量以及根和earth的密度和生物量,并分析了散装土壤的WSA和C以及每个WSA大小分数。杂草地上生物量随场地年龄增加而增加,而凋落物积累,根系生物量(土壤深度为0-4 cm)以及cm密度和生物量似乎与场地年龄无关。与0年相比,NWM第5年的内生o密度和生物量趋于增加。在NWM下,土壤深度为0-15 cm时,WSA> 2 mm,WSA中的土壤C储量> 2 mm随时间增加,而0.25-1-mm WSA的土壤碳储量在0-5 cm的土壤深度下降。在NWM时间序列上,土壤深度为0-25 cm时,土壤总C累积速率为60 g C m -2 yr -1 。因此,我们的结果表明,通过采用NWM,地上杂草对土壤的碳输入以及WSA的增加> 2 mm可能是土壤碳固存的原因。

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