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首页> 外文期刊>Soil Science and Plant Nutrition >Nitrous oxide emissions from green tea fields in Japan: contribution of emissions from soil between rows and soil under the canopy of tea plants
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Nitrous oxide emissions from green tea fields in Japan: contribution of emissions from soil between rows and soil under the canopy of tea plants

机译:日本绿茶园中的一氧化二氮排放量:茶树冠层下行与土壤之间的土壤排放量的贡献

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This study was conducted to assess the contributions of nitrous oxide (N2O) emissions from soil between rows and soil under the canopy of tea plants (Camellia sinensis (L.) Kuntze) to the entire N2O emissions from tea fields and to determine the factors responsible for changes in N2O emissions. The study was performed in an experimental tea field in which fertilizer application rate was 510a??kg nitrogen (N) haa??1a??yra??1. N2O flux and soil properties including temperature, water filled pore space (WFPS), ammonium-nitrogen (-N) and nitrate-nitrogen (-N) concentrations, and soil pH were measured over a period of two years. Total N2O emissions from the entire tea field were 10.6 and 14.8a??kg haa??1a??yra??1 in 2008 and 2009, respectively. Total N2O emissions from soil under the canopy of tea plants were approximately 35% of the total N2O emissions from the entire tea field, suggesting that the contribution of N2O emission from soil under the canopy of tea plants to overall N2O emission was not negligible. A high N2O flux from soil under the canopy was observed when there was heavy rainfall. The key factors for high N2O fluxes observed in soil under the canopy were considered to be increases in soil temperature and WFPS. On the other hand, high N2O fluxes from the soil between rows was observed after fertilizer application in spring and autumn, and there was a significant positive correlation between N2O flux and -N concentration in the soil between rows.View full textDownload full textKeywordsacid soil, fallen leaves, nitrogen cycle, nitrous oxide, tea.Related var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/00380768.2012.686434
机译:本研究旨在评估茶树冠层(茶树)冠层下行和土壤之间的土壤中一氧化二氮(N 2 O)排放对整个N <茶田中的sub> 2 O排放,并确定导致N 2 O排放变化的因素。这项研究是在一个试验性茶园中进行的,肥料用量为510a?kg kg氮(N)ha a ?? 1a ?? yr a ?? 1 。在一段时间内测量N 2 通量和土壤性质,包括温度,充水孔隙空间(WFPS),铵态氮(-N)和硝态氮(-N)的浓度以及土壤pH两年。整个茶田的N 2 O排放总量分别为10.6和14.8a ?? kg ha a ?? 1a ?? yr a ?? 1 分别在2008年和2009年。茶树冠层下土壤的N 2 O排放总量约为整个茶田N 2 O排放总量的35%,这表明N的贡献茶树冠层下土壤的 2 O排放量对总N 2 O排放量的影响不可忽略。暴雨时,冠层下土壤的N 2 O通量较高。冠层下土壤中N 2 O通量高的关键因素被认为是土壤温度和WFPS的升高。另一方面,春季和秋季施肥后,各行间土壤的N 2 O通量较高,N 2 O之间呈显着正相关。行之间土壤中的通量和-N浓度。查看全文下载全文关键字酸性土壤,落叶,氮循环,一氧化二氮,茶。相关变量addadd_config twitter,technorati,美味,linkedin,facebook,stumbleupon,digg,google,更多“,发布:” ra-4dff56cd6bb1830b“};添加到候选列表链接永久链接http://dx.doi.org/10.1080/00380768.2012.686434

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