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不同耕作方式对广西地区甘蔗地土壤热性质的影响

朱彦光 李帅 甘磊 李健 SaeedRad 陈晓冰

朱彦光, 李帅, 甘磊, 李健, SaeedRad, 陈晓冰. 不同耕作方式对广西地区甘蔗地土壤热性质的影响[J]. 福建农业学报, 2019, 34(7): 858-866. doi: 10.19303/j.issn.1008-0384.2019.07.016
引用本文: 朱彦光, 李帅, 甘磊, 李健, SaeedRad, 陈晓冰. 不同耕作方式对广西地区甘蔗地土壤热性质的影响[J]. 福建农业学报, 2019, 34(7): 858-866. doi: 10.19303/j.issn.1008-0384.2019.07.016
ZHU Yan-guang, LI Shuai, GAN Lei, LI Jian, Saeed Rad, CHEN Xiao-bing. Thermal Property of Soil at Sugarcane Fields in Guangxi Affected by Tillage Method[J]. Fujian Journal of Agricultural Sciences, 2019, 34(7): 858-866. doi: 10.19303/j.issn.1008-0384.2019.07.016
Citation: ZHU Yan-guang, LI Shuai, GAN Lei, LI Jian, Saeed Rad, CHEN Xiao-bing. Thermal Property of Soil at Sugarcane Fields in Guangxi Affected by Tillage Method[J]. Fujian Journal of Agricultural Sciences, 2019, 34(7): 858-866. doi: 10.19303/j.issn.1008-0384.2019.07.016

不同耕作方式对广西地区甘蔗地土壤热性质的影响

doi: 10.19303/j.issn.1008-0384.2019.07.016
基金项目: 

国家自然科学基金项目 41501230

国家自然科学基金项目 41761048

国家自然科学基金项目 41701248

广西自然科学基金项目 2017GXNSFBA198102

广西自然科学基金项目 2016GXNSFAA380197

广西中青年教师基础能力提升项目 2017KY0270

详细信息
    作者简介:

    朱彦光(1993-), 男, 硕士研究生, 主要从事农田土壤水热运移研究(E-mail:415024471@qq.com)

    通讯作者:

    陈晓冰(1988-), 男, 博士, 讲师, 主要从事土壤水分运动与模拟研究(E-mail:jayvision_chen@126.com)

  • 中图分类号: S566.1

Thermal Property of Soil at Sugarcane Fields in Guangxi Affected by Tillage Method

  • 摘要:   目的  探讨不同耕作方式下甘蔗地土壤热性质的动态变化,为合理有效利用水热资源提供依据。  方法  在广西农业科学院里建甘蔗种植地进行研究,定位监测粉垄耕作(T)处理和免耕(NT)处理方式下,5、20和40 cm深度土层的土壤含水量和土壤温度,并结合土壤基本参数,分析2个处理下土壤温度、土壤热导率和土壤热通量的变化规律。  结果  NT处理受其质地影响,土壤温度的分布为5 cm > 40 cm > 20 cm,差异均显著(P < 0.05,下同);T处理在一定程度上影响了土壤质地,其土壤温度分布为5 cm > 20 cm > 40 cm,差异均显著。研究期内,T处理土壤热导率在20 cm以上土层高于NT处理。T处理有利于降水入渗、储水性能良好、下层水分可供给上层等效果,相比于NT处理改善了土壤热导率沿土壤剖面的分布。同时,不同降水条件下,处理间的土壤热通量变化相同:NT处理在5~20 cm层大于T处理,而在20~40 cm层小于T处理,差异均达到显著水平。说明T处理土壤热通量由上至下减小,变化规律明显;而NT处理上下层间波动较大。  结论  粉垄耕作处理相比于免耕处理,在一定程度上改善了本地区的土壤质地和土壤温度分布,土壤热导率和土壤热通量的变化更具稳定性和规律性,可作为广西地区农业种植和管理方式的参考。
  • 图  1  不同耕作方式下的土壤温度变化

    Figure  1.  Soil temperature as affected by tillage method

    图  2  不同耕作方式下土壤热导率的变化

    Figure  2.  Changes on soil thermal conductivity under different tillage treatments

    图  3  不同耕作方式下土壤层热通量

    Figure  3.  Heat flux in soil layers under different tillage treatments

    表  1  3种土壤水分条件下土壤的含水量、热导率和热通量

    Table  1.   Moisture content, thermal conductivity, and heat flux rate of soils containing varied amount of water

    试验处理
    Treatments
    土壤水分条件
    Moisture conditions
    5 cm含水量
    Water content of 5 cm soil/(cm3·cm-3)
    5 cm热导率
    Thermal conductivity of 5 cm soil/(W·m-1·K-1)
    5~20 cm热通量Heat flux of 5 cm soil/(W·m-2) 20 cm含水量Water content of 20 cm soil/(cm3·cm-3) 20 cm热导率
    Thermal conductivity of 20 cm soil/(W·m-1·K-1)
    20~40 cm热通量Heat flux of 20-40 cm soil/(W·m-2) 40 cm含水量Water content of 40 cm soil/(cm3·cm-3) 40 cm热导率
    Thermal conductivity of 40 cm soil/(W·m-1·K-1)
    T 湿润条件Wetmoisture conditions 0.309±0.010Ac 1.323±0.019Ac -182.656±42.483Ba 0.343±0.014Ab 1.355±0.022Ab -145.080±19.061Aa 0.383±0.014Aa 1.411±0.022Aa
    中等水分条件
    Mediummoisture conditions
    0.304±0.007Aa 1.315±0.012Aa -101.966±33.968Ba 0.275±0.007Ab 1.243±0.012Ab -120.840±18.035Aa 0.322±0.011Aa 1.300±0.017Aa
    干旱条件
    Dry moisture conditions
    0.295±0.007Aa 1.272±0.011Aa -71.772±33.041Aa 0.268±0.007Ac 1.223±0.011Ab -50.002±17.196Ba 0.276±0.009Bb 1.202±0.012Bb
    NT 湿润条件
    Wetmoisture conditions
    0.315±0.008Ab 1.348±0.014Aa -347.129±50.110Aa 0.290±0.019Bc 1.240±0.032Bc 11.751±13.669Bb 0.367±0.011Aa 1.410±0.018Aa
    中等水分条件
    Mediummoisture conditions
    0.287±0.008Bb 1.297±0.013Bb -257.018±31.863Aa 0.240±0.008bc 1.153±0.015Bc 51.766±14.054Bb 0.330±0.007Aa 1.336±0.011Aa
    干旱条件
    Dry moisture conditions
    0.260±0.004Bb 1.241±0.002Bb 13.574±25.967Bb 0.220±0.007Bc 1.113±0.011Bc -89.052±17.074Aa 0.306±0.006Aa 1.302±0.008Aa
    注:表中不同大写字母表示同一水分条件和同一深度下不同处理间的差异显著(P < 0.05);不同小写字母表示同一处理和同一水分条件下不同土层深度下的差异显著(P < 0.05)。
    Note:Different capital letters indicated significant difference under different tillage patterns when the water conditions and soil depths are the same (P < 0.05); different small letters indicated significant difference under different soil depths when the tillage patterns and water conditions are the same (P < 0.05).
    下载: 导出CSV
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  • 收稿日期:  2019-05-25
  • 修回日期:  2019-06-22
  • 刊出日期:  2019-07-20

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