首页> 外文期刊>Nutrient Cycling in Agroecosystems >Increase of N_2O fluxes in agricultural peat and sandy soil under elevated CO_2 concentration:concomitant changes in soil moisture,groundwater table and biomass production of Phleum pratense
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Increase of N_2O fluxes in agricultural peat and sandy soil under elevated CO_2 concentration:concomitant changes in soil moisture,groundwater table and biomass production of Phleum pratense

机译:CO_2浓度升高时农业泥炭和沙质土壤N_2O通量的增加:土壤水分,地下水位和of草生物量的变化

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摘要

The effects of elevated atmospheric CO_2 concentration on soil moisture,N_2O fluxes,and biomass production of Phleum pratense were studied in the laboratory.Farmed peat and sandy soil mesocosms sown with P.pratense were fertilized with a commercial fertilizer.In peat soil 10 g N m~(-2) of commercial fertilizer were added and in sandy soil 15 g N m~(-2).In both experiments,soil moisture was regulated with deionized water;18 mesocosms were tended to keep equally moist,and the other 18 were watered with equal amounts of water.Nine mesocosms from both watering treatments were grown under ambient (360 mu mol mol~(-1)) CO_2 concentration and the remaining nine under doubled (720 mu mol mol~(-1)) CO_2.N_2O efflux was monitored using a closed chamber technique and a gas chromatograph.The elevated supply of CO_2 increased production of above-and belowground biomass,soil moisture and N_2O fluxes,but decreased the total N content in the aboveground biomass,especially for the sandy soil.In similar water levels,N_2O efflux from the sandy soil was the same magnitude as that from the peat soil.In addition to moisture,N availability was the main limiting factor for N_2O production,but C availability also seemed to regulate the denitrification activity.In addition to an increase in C availability the increase in the N_2O efflux under the raised CO_2 concentration also required a simultaneous increase in soil moisture.
机译:在实验室中研究了大气中CO_2浓度升高对p草的土壤水分,N_2O通量和生物量产生的影响。对种有P.pratense的农作物泥炭和沙质土壤包膜进行了商业化肥施肥。在泥炭土中10 g N添加了m〜(-2)的商品肥料,并在沙土中添加了15 g N m〜(-2)。在这两个实验中,均用去离子水调节了土壤的水分;倾向于使18个中膜保持同样的湿润,另外18个两种浇水处理的九个中观膜均在环境(360μmolmol〜(-1))CO_2浓度下生长,其余九种在两倍的(720μmolmol〜(-1))CO_2下生长。使用密闭室技术和气相色谱仪监测N_2O的流出量。增加的CO_2供应量增加了地上和地下生物量,土壤水分和N_2O通量的产量,但降低了地上生物量中的总N含量,特别是对于沙土。类似水分水平,沙土的N_2O流出量与泥炭土的流出量相同。除水分外,氮的有效性是限制N_2O产生的主要因素,但碳的有效性似乎也调节了反硝化活性。碳的有效性增加,在CO_2浓度升高的情况下,N_2O外排量的增加也需要土壤水分的同时增加。

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