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首页> 外文期刊>Global Biogeochemical Cycles >Contribution of winter soil respiration to annual soil CO _2 emission in a Mollisol under different tillage practices in northeast China
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Contribution of winter soil respiration to annual soil CO _2 emission in a Mollisol under different tillage practices in northeast China

机译:东北地区不同耕作方式下冬季土壤呼吸对毛囊土壤CO _2排放的贡献

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Winter soil CO _2 emission is a very important component of the annual carbon budgets, however, almost no information on winter CO _2 emission is available from the cropland soil in northeast China. In this study, soil CO _2 flux was measured for a 2-year period from an ongoing tillage trial on Black soil in northeast China to quantify seasonal patterns in soil CO _2 flux rate and wintertime contribution to annual soil respiration. Average soil CO _2 flux rates in the winter (November to March) were between 0.64 to 1.22 g CO _2 m -2 d ~(-1), in the non-growing season (October and April) were 2.09-3.56 g CO _2 m -2 d ~(-1), whereas in the growing season (May to September) they were between 10.9 to 12.7 g CO _2 m ~(-2) d ~(-1), with no significant differences among tillage treatments. Total winter, non-growing and growing season soil CO _2 emissions were 0.28-0.45 Mg C ha ~(-1), 0.36-0.53 Mg C ha ~(-1), and 4.52-5.55 Mg C ha ~(-1), respectively, among tillage treatments. The contributions of winter soil respiration to annual soil CO _2 emission ranged from 5.1 to 7.1%, and the non-growing season emission ranged from 11.4 to 15.2% among tillage treatments. Our results indicate that in northeast China, cropland Black soil continuously emits CO _2 throughout the non-growing season, and the wintertime soil respiration plays a significant role in annual soil carbon budgets. Hence winter soil CO _2 emission must be taken into consideration when the role of the soil ecosystem is assessed as either a sink or source of CO _2 to the atmosphere.
机译:冬季土壤CO _2排放是年度碳预算中非常重要的组成部分,但是,在中国东北的农田土壤中几乎没有关于冬季CO _2排放的信息。在这项研究中,从正在进行的中国东北黑土耕作试验中测量了为期2年的土壤CO _2通量,以量化土壤CO _2通量率的季节性模式以及冬季对年度土壤呼吸的贡献。冬季(11月至3月)的平均土壤CO _2通量率在0.64至1.22 g CO _2 m -2 d〜(-1)之间,在非生长季节(10月和4月)为2.09-3.56 g CO _2 m -2 d〜(-1),而在生长季节(5月至9月)则在10.9至12.7 g CO _2 m〜(-2)d〜(-1)之间,耕作处理之间无显着差异。整个冬季,非生长季节和生长季节的土壤CO _2排放分别为0.28-0.45 Mg C ha〜(-1),0.36-0.53 Mg C ha〜(-1)和4.52-5.55 Mg C ha〜(-1)分别在耕作处理中。在耕作处理中,冬季土壤呼吸对年土壤CO _2排放的贡献为5.1%至7.1%,非生长季节排放的贡献为11.4%至15.2%。我们的结果表明,在中国东北,农田黑土在整个非生长季节持续排放CO _2,而冬季土壤呼吸作用在年度土壤碳收支中起着重要作用。因此,当评估土壤生态系统的作用是向大气中吸收或吸收CO _2时,必须考虑冬季土壤中的CO _2排放。

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