红寺堡酿酒葡萄根系层冬季土壤温度变化特征  被引量:3

Winter Soil Temperature Changes in the Root Layer of Hongsibu Wine Grape

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作  者:杜宏娟 赵斯文[3] 魏月娥 张磊 李娜[3] Du Hongjuan;Zhao Siwen;Wei Yue'e;Zhang Lei;Li Na(Key Laboratory for Meteorological Disaster Monitoring and Early Warning and Risk Management of Characteristic Agriculture in in Arid Regions,China Meteorological Administration,Yinchuan 750002;Ningxia Key Lab of Meteorological Disaster Prevention and Reduction,Yinchuan 750002;Wuzhong Meteorological Office,Wuzhong Ningxia 751100)

机构地区:[1]中国气象局旱区特色农业气象灾害监测预警与风险管理重点实验室,银川750002 [2]宁夏气象防灾减灾重点实验室,银川750002 [3]吴忠市气象局,宁夏吴忠751100

出  处:《中国农学通报》2018年第34期103-107,共5页Chinese Agricultural Science Bulletin

基  金:国家自然科学基金"贺兰山东麓酿酒葡萄晚霜冻预报方法研究"(41465004);中国气象局旱区特色农业气象灾害监测预警与风险管理重点实验室开放项目"红寺堡酿酒葡萄冬季根系层土壤温度预报研究"

摘  要:为全面掌握红寺堡酿酒葡萄根系层冬季土壤温度的变化特征,利用同心气象站1961—2015年冬季(12月—次年2月)0、10、15、20、40 cm逐日平均土壤温度资料,对其变化规律分析。结果表明:酿酒葡萄根系层冬季土壤温度垂直变化特点是随着深度增加呈升高趋势;55年冬季0~40 cm平均土壤温度日变化趋势一致,先降后升,最低值在-7.3^-3.4℃之间,出现时间在1月13—25日;55年冬季土壤温度年际变化呈显著上升趋势;0~20 cm各层气候变化倾向率在0.432~0.604℃/10 a,0、5、10、20 cm土壤温度分别在1989年、1989年、1989年、1984年发生了突变,突变前均为冷期,突变后均为暖期;55年冬季土壤温度年代际变化总体以升温为主,21世纪10年代较21世纪00年代呈下降趋势。To study winter soil temperature changes in root layer of Hongsibu wine grape,the variation law was analyzed by using daily average soil temperature data of 0,10,15,20 and 40cm (December to next February) from 1961 to 2015 of Tongxin weather station.The results showed that soil temperature in the root layer increased with the increase of depth;the daily average variation in 0-40cm soil layers of the 55years had the same trend of first decreasing and then increasing,with the lowest value ranging from -7.3℃ to -3.4℃ and the appearance time between January 13 and January 25.The inter-annual variation had a significant increasing trend in the 55 years.In 0-20cm,climate change tendency rate of each layer was between 0.432-0.604℃/10a. The soil temperature of 0,5,10and 20cm respectively had a mutation in 1989,1989,1989and 1984,all of them were cold periods before mutation,warm after mutation.The inter-decadal variation was mainly temperature rising,but the 2010s showed a declining trend compared with the 2000s.

关 键 词:酿酒葡萄 根系层 土壤温度 变化特征 

分 类 号:S161.9[农业科学—农业气象学]

 

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