globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6057463
论文题名:
增温和降水减少对冬小麦和大豆生长季土壤氮素的影响
其他题名: Effects of Diurnal Warming and Reduced Precipitation on Soil Nitrogen in Winter-wheat and Soybean Growing Season
作者: 陈健1; 王艺杰2; 胡正华1; 王亚萍2; 陈书涛1; 胡冰冰3; 李雯雯2; 杨蕙琳2; 李凯丽2
刊名: 生态环境学报
ISSN: 1674-5906
出版年: 2017
卷: 26, 期:7, 页码:387-395
语种: 中文
中文关键词: 增温 ; 降水减少 ; 冬小麦 ; 大豆 ; 全氮 ; 铵态氮 ; 硝态氮
英文关键词: diurnal warming ; reduced precipitation ; winter wheat ; soybean ; total nitrogen ; NH_4~+-N ; NO_3~--N
WOS学科分类: ENVIRONMENTAL SCIENCES
WOS研究方向: Environmental Sciences & Ecology
中文摘要: 氮素是农田土壤的主要养分限制因子之一,在全球气候变化背景下研究农田土壤氮素对温度和降水变化的响应,对评价气候变化农业生态效应具有重要的意义。通过田间试验,利用红外辐射灯管模拟增温,人工减少降水量,并测定土壤氮素含量,以探讨增温和降水减少对冬小麦和大豆生长季土壤氮素的影响规律。试验设置对照(CK)、增温(T,增温约2 ℃)、降水减少(P,降水量减少30%)、增温和降水减少复合处理(TP,增温约2 ℃+降水减少30%)4个水平处理。结果表明,在冬小麦生长季,与CK相比,T、P和TP处理显著减少了返青期土壤全氮,增加了成熟期土壤全氮;T和TP处理显著降低了拔节期土壤全氮。T、P和TP处理显著减少了孕穗-抽穗期土壤铵态氮。P和TP处理显著增加了返青-灌浆期土壤硝态氮,T处理显著增加了拔节-抽穗期土壤硝态氮。在大豆生长季,与CK相比,T、P和TP处理对土壤全氮含量的影响都没有达到显著性水平。T处理使鼓粒期土壤铵态氮增加10.0%(P=0.038),T和P处理使结荚期土壤硝态氮分别减少了27.4%(P=0.011)和27.1%(P=0.009),T、P和TP使鼓粒期土壤硝态氮分别增加了46.6%(P=0.007)、41.3% (P=0.014)和56.3%(P=0.003)。研究表明,增温和降水减少改变了农田土壤氮素含量,且对冬小麦生长季土壤氮素的影响较大豆生长季更加明显。
英文摘要: Nitrogen is one of the main nutrient limiting factors in farmland soils. The study on the response of soil nitrogen to temperature and precipitation changes under the scenario of global climate change, will have a great significance to evaluate the ecological effects of climate change on agriculture. To investigate the effect of warming and reduced precipitation on soil nitrogen, field experiments with simulation warming using infrared lamp radiation and artificial reduction of precipitation were conducted in the 2015-2016 winter-wheat and soybean growing season. The experimental treatments included the control (CK), diurnal warming (T, about enhanced 2 ℃), 30% reduced precipitation (P), and the combined treatment (TP, warming about 2 ℃ plus 30% reduced precipitation). The results showed that in the winter wheat-growing season, compared to CK, T, P and TP treatments significantly reduced soil total nitrogen in the turning green stage, and significantly increased soil total nitrogen in the maturity stage. T and TP treatments significantly reduced soil total nitrogen in the elongation stage. T, P and TP treatments significantly reduced soil NH_4~+-N in the booting-heading stage. P and TP treatments significantly increased soil NO_3~--N in the turning green - grain filling stage, and T treatment significantly increased soil NO_3~--N in the elongation - heading stage. In the soybean-growing season, compared to CK, T, P and TP treatments had no significant effect on soil total nitrogen. T treatment significantly increased soil NH_4~+-N by 10.0% (P=0.038) in the grain-filling stage. T and P treatments significantly reduced the soil NO_3~--N by 27.4% (P=0.011) and 27.1% (P=0.009) in the podding stage, respectively. T, P and TP treatments significantly increased soil NO_3~--N by 46.6% (P=0.007), 41.3% (P=0.014) and 56.3% (P=0.003) in the grain-filling stage, respectively. Our findings suggest that warming and reduced precipitation may alter soil nitrogen content of farmland, and there is an more obvious effect on soil nitrogen in winter-wheat farmland than in soybean farmland.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/152896
Appears in Collections:气候变化事实与影响

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作者单位: 1.南京信息工程大学, 气象灾害预报预警与评估协同创新中心
2.江苏省农业气象重点实验室, 南京, 江苏 210044, 中国
3.南京信息工程大学应用气象学院, 南京, 江苏 210044, 中国
4.南京外国语学校, 南京, 江苏 210008, 中国

Recommended Citation:
陈健,王艺杰,胡正华,等. 增温和降水减少对冬小麦和大豆生长季土壤氮素的影响[J]. 生态环境学报,2017-01-01,26(7):387-395
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