期刊文献+

Effects of nitrogen addition on carbonate-derived CO_(2) emission after biochar addition

原文传递
导出
摘要 ●We studied the effect of nitrogen and biochar on CO_(2) emission from SOC and SIC.●Nitrogen increased SIC-derived CO_(2) by 41%but decreased SOC-derived CO_(2) by 20%.●Biochar reduced total soil-derived CO_(2) by neutralizing nitrogen-induced acidity.●We proposed a method for 3-or 4-source partitioning CO_(2) emission from calcareous soils.Biochar addition generally increases the alkalinity regeneration to resist soil acidification driven by nitrogen(N)fertilization.Calcareous soils contain soil organic carbon(SOC)and inorganic C(SIC).Owing to technical limitations in three-source partitioning CO_(2),how biochar addition affects SOC-and SIC-derived CO_(2) emission has not been clarified yet.Therefore,we conducted a 70-day incubation experiment of ammonium-N and maize-straw-derived biochar additions to investigate the N plus biochar impacts on SOC-and SIC-derived CO_(2) emission.Over the 70-day incubation,we found that the N-only addition increased the SIC-derived CO_(2) emission by approximately 41%compared with the control,but decreased the SOC-derived CO_(2) emission by approximately 20%.This suggests that the distinct responses of SIC-and SOC-derived CO_(2) emission to N-only addition come from N-induced acidification and preferential substrate(N)utilization of soil microorganisms,respectively.Compared with N-only addition,N plus biochar addition decreased the SIC-derived CO_(2) emission by 17%−20%during the first 20 days of incubation,but increased it by 54%during the next 50 days.This result suggested that biochar addition reduced the SIC-derived CO_(2) emission likely due to the alkalization capacity of biochar exceeding the acidification capacity of ammonium-N in the short term,but it may increase the SIC-derived CO_(2) emission induced by the weak acidity produced from biochar mineralization in the long term.This study is helpful to improve the quantification of CO_(2) emission from calcareous soils.
出处 《Soil Ecology Letters》 CSCD 2023年第4期39-49,共11页 土壤生态学快报(英文)
基金 supported by the National Natural Science Foundation of China(32072518 and 42141006) the Natural Science Foundation of Shandong Province(ZR2020QD042).
  • 相关文献

参考文献6

二级参考文献33

  • 1JU Xiao-Tang,LIU Xue-Jun,PAN Jia-Rong,ZHANG Fu-Suo.Fate of ^(15)N-Labeled Urea Under a Winter Wheat-Summer Maize Rotation on the North China Plain[J].Pedosphere,2007,17(1):52-61. 被引量:44
  • 2全国土壤普查办公室.中国土种志(1-6卷)[M].北京:中国农业出版社,1993,1994a,1994b,1995a,1995b..
  • 3Schlesinger W H. The formation of caliche in soils of the Mojave Desert, California. Geochimica et Cosmochimica Acta, 1985, 49 (1) : 57-66.
  • 4Hastings S J, Oechel W C, Muhlia-Melo A. Diurnal, seasonal and annual variation in the net ecosystem C02 exchange of a (Sarcocaulescent) in Baja Ca Change Biology, 2005 desert shrub community lifo rnia, Mexico. Global 927-939.
  • 5Wohlfahrt G L, Fenstermaker F, Arnone J A. Large annum net ecosystem CO2 uptake of a Mojave Desert ecosystem. Global Change Biology, 2008, 14 (7) : 1475-1487.
  • 6Xie J X, Li Y, Zhai C X, el al. C02 absorption by alkaline soils and its implication to the global carbon cycle. Environmental Geology, 2009, 56 ( 5 ) : 953- 961.
  • 7Stone R. Have desert researchers discovered a hidden loop in the carbon cycle.'? Science, 2008, 320 (5882) : 1409-1410.
  • 8Schlesinger W H, Belnap J, Marion G. On carbon sequestration in desert ecosystems. Global Change Biology, 2009, 15 (6) : 1488-1490.
  • 9Ma J, Wang Z Y, Stevenson B A, et al. An inorganic COz diffusion and dissolution process explains negative CO2 fluxes in saline/alkaline soils. Scientific Reports, 2013. 3, 2025.
  • 10Hamerlynck E P, Scott R L, Snchez-Cafiete E P, et al. Nocturnal soil CO2 uptake and its relationship to subsurface soil and ecosystem carbon fluxes in a Chihuahuan Desert shrubland. ournal of Geophysical Research: Biogeosciences, 2013, 118 (4) : 1593- 1603.

共引文献369

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部