山西省农业科学院小麦研究所,山西,临汾,041000
纸质出版:2020
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靖华, 马爱平, 亢秀丽, 等. 黄淮海北片模拟增加和降低温度对麦田地温、水分变化和水分利用效率的影响[J]. 水土保持学报, 2020,34(1):217-224.
JING Hua, MA Aiping, KANG Xiuli, et al. Effects of Simulated Temperature Increase and Decrease on Ground Temperature, Soil Moisture Change, and Water Use Efficiency in the North of Huang-Huai-Hai Wheat Field[J]. 2020, 34(1): 217-224.
靖华, 马爱平, 亢秀丽, 等. 黄淮海北片模拟增加和降低温度对麦田地温、水分变化和水分利用效率的影响[J]. 水土保持学报, 2020,34(1):217-224. DOI: 10.13870/j.cnki.stbcxb.2020.01.031.
JING Hua, MA Aiping, KANG Xiuli, et al. Effects of Simulated Temperature Increase and Decrease on Ground Temperature, Soil Moisture Change, and Water Use Efficiency in the North of Huang-Huai-Hai Wheat Field[J]. 2020, 34(1): 217-224. DOI: 10.13870/j.cnki.stbcxb.2020.01.031.
采用模拟增降温法研究了温度变化对麦田地温、土壤水分变化和水分利用效率的影响。结果表明:模拟增温麦田、降温麦田在全生育期5 cm平均地温分别较常规麦田平均升高0.85℃和降低2.57℃,其中模拟增温麦田的增温效应以冬季 > 秋季 > 春季,模拟降温麦田的降温效应以春季 > 秋季 > 冬季;模拟增温麦田、降温麦田在全生育期5 cm土层的平均容积含水率分别较常规麦田降低3.76%、提高4.84%。对模拟增温麦田、降温麦田和常规麦田0-200 cm土层水分变化研究表明,模拟增温麦田和常规麦田(除成熟期外)各生育期的贮水量均低于模拟降温麦田;全生育期0-200 cm土层土壤耗水量模拟增温麦田大于模拟降温麦田和常规麦田,其中0-100 cm土层耗水量占0-200 cm土层耗水量的比例模拟增温麦田(55.72%)和常规麦田(55.14%)均低于模拟降温麦田(63.45%),而100-200 cm土层耗水量占0-200 cm土层耗水量的比例模拟增温麦田(44.28%)和常规麦田(44.86%)麦田均高于模拟降温麦田(36.55%);水分利用效率模拟增温麦田低于常规麦田和模拟降温麦田。研究结果可为气候变暖对小麦生产系统的影响提供理论依据和技术支撑。
The effects of temperature change on wheat field temperature
soil moisture change
and water use efficiency were studied by simulated temperature increase and decrease method. The results showed that the average 5 cm ground temperature of the warming wheat field and the cooling wheat field in the whole growth period increased by 0.85 oC and decreased by 2.57 oC
respectively
compared with the conventional wheat field. The simulated warming effect of the warming wheat field was winter > autumn > spring
and the simulated cooling effect of the cooling wheat field was spring > autumn > winter. The average volumetric water content of 5 cm soil layer in the whole growth period of the simulated warming and cooling wheat field was 3.76% lower and 4.84% higher than that of conventional wheat field
respectively. The study of soil water change in 0-200 cm soil layer of simulated warming
cooling wheat field
and conventional wheat field showed that the water storage of simulated warming and conventional wheat field (except mature stage) was lower than that of simulated cooling wheat field at all growth stages; the water consumption in 0-200 cm soil layer during whole growth period in warming wheat field was higher than that in simulated cooling and conventional wheat field
of which the proportion of 0-100 cm water consumption to 0-200 cm in simulated warming wheat field (55.72%) and conventional wheat field (55.14%) was lower than that of simulated cooling wheat field (63.45%)
while the proportion of water consumption of 100-200 cm to 0-200 cm in simulated warming wheat field (44.28%) and conventional wheat field (44.86%) was higher than that of simulated cooling wheat field (36.55%). The water use efficiency of simulated warming wheat field was lower than that of conventional wheat field and simulated cooling wheat field. This study can provide theoretical basis and technical support for the impact of climate warming on wheat production system.
秦大河.气候变化与干旱[J].科技导报,2009,27(11):3.
任国玉,徐铭志,初子莹,等.近54年中国地面气温变化[J].气候与环境研究,2005,10(4):717-727.
张卉,郭慕萍,赵双巧,等.1960-2008年山西省气温变化特征[J].气象与环境学报,2012,28(2):16-21.
苗爱梅,武捷,贾利冬.1958-2008年山西气温变化的特征及趋势研究[J].地球科学进展,2010,25(3):264-272.
费晓玲,丁春兰.甘肃黄土高原地温与冬小麦发育期的关系分析[J].干旱气象,2009,27(2):148-151.
王春玲,申双和,王润元,等.天水地区冬春地温变化与冬小麦生长和产量的相关分析[J].干旱地区农业研究,2012,30(5):41-45.
刘新月,裴磊,卫云宗,等.气温变化背景下中国黄淮旱地冬小麦农艺性状的变化特征:以山西临汾为例[J].中国农业科学,2015,48(10):1942-1954.
唐晓培,宋妮,陈智芳,等.黄淮海地区冬小麦种植北界时空演变及未来趋势分析[J].农业工程学报,2019,35(9):129-137.
周英霞,王全九,何斌,等.气温和CO
2
浓度变化对陕北地区冬小麦产量影响的模拟分析[J].水土保持学报,2017,31(5):292-297.
周林,王汉杰,朱红伟.气候变暖对黄淮海平原冬小麦生长及产量影响的数值模拟[J].解放军理工大学学报:自然科学版,2003,4(2):76-82.
杨轩,王自奎,曹铨,等.陇东地区几种旱作作物产量对降水与气温变化的响应[J].农业工程学报,2016,32(9):106-114.
靖华,亢秀丽,马爱平,等.不同海拔麦田土壤水分变化特征及其对水分利用效率的影响[J].干旱气象,2019,37(4):656-662.
牛书丽,韩兴国,马克平,等.全球变暖与陆地生态系统研究中的野外增温装置[J].植物生态学报,2007,31(2):262-271.
张凯,王润元,王鹤龄,等.模拟增温对半干旱雨养区春小麦物质生产与分配的影响[J].农业工程学报,2016,32(16):223-232.
冯学民,蔡德利.土壤温度与气温及纬度和海拔关系的研究[J].土壤学报,2004,41(3):489-491.
Hartley A E, Neill C, Melillo J M, et al. Plant performance and soil nitrogen mineralization in response to simulated climate change in subarctic dwarf heath[J]. Oikos,1999,86:331-343.
Bergh J, Linder S. Effects of soil warming during spring on photosynthetic recovery in boreal Norway spruce stands[J]. Global Change Biology,1999,5:245-253.
唐启义,冯明光.实用统计分析及其DPS数据处理系统[M].北京:科学出版社,2002.
任国玉,郭军,徐铭志,等.近50年中国地面气候变化基本特征[J].气象学报,2005,63(6):942-956.
田云录,郑建初,张彬,等.麦田开放式昼夜不同增温系统的设计及增温效果[J].中国农业科学,2010,43(18):3724-3731.
申双和,盛琼.45年来中国蒸发皿蒸发量的变化特征及其成因[J].气象学报,2008,66(3):452-460.
亢秀丽,靖华,马爱平,等.区域(临汾)水分相关气象因子变化及其对小麦产量的影响[J].农学学报,2019,9(7):62-67
Kimball B A. Theory and performance of an infrared heater for ecosystem warming[J]. Global Change Biology,2005,11:2041-2056.
Zavaleta E S, Thomas B D, Chiariello N R, et al. Plants reverse warming effect on ecosystem water balance[J]. Proceedings of the National Academy of Sciences,2003,100:9892-9893.
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