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      氣候變化研究進展 ?? 2012, Vol. 8 ?? Issue (4): 265-271.

      ? 氣候變化影響 ? 上一篇    下一篇

      北方農牧交錯帶春小麥生育期對氣候變化的響應——以內蒙古武川縣為例

      董智強1,2, 潘志華1,2, 安萍莉1, 潘學標1,2, 趙沛義2   

      1. 1 中國農業(yè)大學資源與環(huán)境學院;
        2 農業(yè)部呼和浩特農牧交錯帶生態(tài)環(huán)境重點野外科學觀測試驗站
      • 收稿日期:2011-10-14 修回日期:2012-02-20 出版日期:2012-07-30 發(fā)布日期:2012-07-30
      • 通訊作者: 潘志華 E-mail:panzhihua@cau.edu.cn
      • 基金資助:

        國家自然科學基金資助項目;國家重大科學研究計劃“973”項目

      Responses of Growth Period of Spring Wheat in Northern Ecotone to Climate Change: A Case of Wuchuan County, Inner Mongolia, China

      • Received:2011-10-14 Revised:2012-02-20 Online:2012-07-30 Published:2012-07-30

      摘要: 北方農牧交錯帶是氣候變化的敏感地帶,研究氣候變化對農業(yè)生產的影響規(guī)律與農業(yè)生產的響應特征,對促進北方農牧交錯帶的農業(yè)可持續(xù)發(fā)展具有重要意義。以北方農牧交錯帶代表性站點——武川縣為例,基于1960—2009年氣象觀測數(shù)據和1992—2010年春小麥農業(yè)氣象觀測數(shù)據,研究了氣候變化與春小麥生育期變化之間的相互關系。結果表明,武川縣1960—2009年年平均氣溫每10年升高0.43℃,春季穩(wěn)定通過0℃的初日每10年提前0.98 d,當?shù)貪M足春小麥播種溫度的日期有提前的趨勢,秋季穩(wěn)定通過0℃的終日每10年推遲0.24 d,生長季具有延長趨勢;1992—2010年作物生長季(4—8月)0~10 cm、10~20 cm土壤相對濕度有明顯下降趨勢,平均每10年分別下降18%和13%;播種期與0~10 cm和10~20 cm土壤相對濕度呈現(xiàn)顯著負相關關系,表現(xiàn)為土壤相對濕度每降低1%,播種期分別推遲0.2 d和0.3 d;各生育期與播種期一樣,受溫度與水分綜合作用的影響,不同生育期與二者之間關系不同,各生育期之間持續(xù)日數(shù)與二者呈正相關關系。研究得出,春小麥生育期的變化是各氣侯因素綜合作用的結果,在北方農牧交錯帶,水分對農作物生長發(fā)育具有較大影響,直接影響著春小麥的各個生育過程。

      關鍵詞: 氣候變化, 春小麥, 生育期, 響應, 武川縣

      Abstract: The northern ecotone is an area sensitive to climate changes, and crop’s growth and development are profoundly affected by them. Studies on the impact law of climate change on agricultural production and crops’ response to climate change are of great significance to promote sustainable development of agriculture in the northern farming-pastoral ecotone. Based on the 1960-2009 meteorological data and 1992-2010 agro-meteorological observation data of spring wheat in Wuchuan County, the relationship between climate change and growth period changes of spring wheat were studied in this paper as a representative case of the northern farming-pastoral ecotone. It is shown that the annual temperature of Wuchuan County increased at an average rate of 0.43℃/10a in 1960-2009. The date to meet the spring wheat seeding temperature had an advanced trend. The first date for daily mean temperature in spring to steadily pass through 0 ℃ advanced 0.98 d/10a, the last date for daily mean temperature in autumn to steadily fall down through 0 ℃ postponed 0.24 d/10a, and thereby the growing season of spring wheat had an extending trend. The soil relative humidity in soil layers 0-10 cm and 10-20 cm depth in crop growing season (April-August) during the period 1992-2010 had a decreasing trend with an average rate of 18%/10a and 13%/10a, respectively. The first date of the sowing stage was significantly negatively correlated with the soil relative humidity of 0-10 cm and 10-20 cm depths, i.e., the soil relative humidity reduced every 1%, the first date delayed 0.2 and 0.3 d, respectively. The other growing stages were the same as sowing stage, affected by the combined effects of temperature and soil moisture, that is to say, duration days between various growth stages was positively correlated with temperature and soil moisture. It is concluded that changes in spring wheat growth period are the result of the combined effect of climatic factors, but in the northern farming-pastoral ecotone, soil moisture has a greater impact on crop’s growth and development, in particular, directly on all growth stage processes of spring wheat.

      Key words: climate change, spring wheat, growth period, response, Wuchuan County

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