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中国农学通报

中国农学通报 ›› 2016, Vol. 32 ›› Issue (36): 120-124.doi: 10.11924/j.issn.1000-6850.casb16050166

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

新疆国家一级农试站多年土壤湿度特征分析

韩春光1,张 玲2,任 岗1,蒲云锦1   

  1. (1新疆石河子气象局,新疆石河子 832000；2乌兰乌苏农业气象试验站,新疆石河子 832000）
  • 收稿日期:2016-05-29 修回日期:2016-06-25 接受日期:2016-07-15 出版日期:2016-12-26 发布日期:2016-12-26
  • 通讯作者: 张玲
  • 基金资助:
    石河子垦区蟠桃花期霜冻灾害气象指标研究(MS201610)。

Soil Moisture for Years in Xinjiang National Agricultural Test StationHan Chunguang1, Zhang Ling2, Ren Gang1, Pu Yunjin1

(1Shihezi Meteorological Bureau, Shihezi Xinjiang 832000；   

  1. 2Wulanwusu Agricultural Meteorological Test Station, Shihezi Xinjiang 832000)
  • Received:2016-05-29 Revised:2016-06-25 Accepted:2016-07-15 Online:2016-12-26 Published:2016-12-26

PDF (PC)

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摘要： 为了给新疆石河子垦区农业可持续发展、合理开展农业生产和气候资源利用等提供气候依据，笔者统计分析了新疆石河子国家一级农试站1996—2015年20年来0~50 cm月平均土壤湿度、年平均土壤湿度变化特征及与其他气象因子的相关性。结果表明：0~50 cm年平均土壤湿度总体呈偏湿趋势；石河子国家一级农试站0~10 cm月平均土壤湿度3月和4月湿度最大，6月、7月和8月湿度最小，随着土壤深度的增加，土壤湿度各月相差不大；0~10 cm年平均土壤湿度变化存在着准13年的年代际周期和准5年的年际周期，40~50 cm年平均土壤湿度存在着准10年的年代际周期和准5年的年际周期；0~10 cm和10~20 cm年均土壤湿度存在突变特征；0~50 cm年平均土壤湿度与年降水量、年蒸发量和年0 cm地温这些气象因子最为敏感。

关键词: 棉花, 棉花, 增产, 延迟吐絮, 棉桃收获机

Abstract: To provide climatic information for agricultural sustainable development, and reasonable utilization of agricultural and climate resources in Shihezi, Xinajing, the authors statistically analyzed 0-50 cm monthly average soil moisture, annual average soil moisture and its correlation with other meteorological factors in Xinjiang national agriculture test station from 1996 to 2015. The results showed that: 0-50 cm monthly average soil moisture overall showed a trend of wet; 0-10 cm monthly average soil moisture in March and April were the largest, the smallest humidity was found in June, July and August, with the increase of soil depth, soil moisture had little difference between each month; the change of 0-10 cm annual average soil moisture had a decadal cycle of 13 years and an annual cycle of 5 years, the change of 40-50 cm annual average soil moisture had a decadal cycle of 10 years and an annual cycle of 5 years; the characteristic of 0-10 cm and 10-20 cm annual average soil moisture had mutations; 0-50 cm annual average soil moisture was most sensitive to the meteorological factors of annual precipitation, annual evaporation and annual 0 cm ground temperature.