毛妍婷, 崔荣阳, 陈安强, 平凤超, 雷宝坤. 垄作方向对不同坡位红壤坡耕地耕层土壤水分特征曲线的影响[J]. 土壤通报, 2022, 53(2): 308 − 314. DOI: 10.19336/j.cnki.trtb.2021042801
引用本文: 毛妍婷, 崔荣阳, 陈安强, 平凤超, 雷宝坤. 垄作方向对不同坡位红壤坡耕地耕层土壤水分特征曲线的影响[J]. 土壤通报, 2022, 53(2): 308 − 314. DOI: 10.19336/j.cnki.trtb.2021042801
MAO Yan-ting, CUI Rong-yang, CHEN An-qiang, PING Feng-chao, LEI Bao-kun. Effects of Ridge Directions on Water Characteristic Curves of Cultivated Top-Layer Soils in Different Slope Positions[J]. Chinese Journal of Soil Science, 2022, 53(2): 308 − 314. DOI: 10.19336/j.cnki.trtb.2021042801
Citation: MAO Yan-ting, CUI Rong-yang, CHEN An-qiang, PING Feng-chao, LEI Bao-kun. Effects of Ridge Directions on Water Characteristic Curves of Cultivated Top-Layer Soils in Different Slope Positions[J]. Chinese Journal of Soil Science, 2022, 53(2): 308 − 314. DOI: 10.19336/j.cnki.trtb.2021042801

垄作方向对不同坡位红壤坡耕地耕层土壤水分特征曲线的影响

Effects of Ridge Directions on Water Characteristic Curves of Cultivated Top-Layer Soils in Different Slope Positions

  • 摘要:
      目的  探讨横坡垄作和顺坡垄作对不同坡位耕层土壤水分特征曲线的影响,为红壤坡耕地垄作方向的选择提供依据。
      方法  采用压力膜仪法测定两种垄作方向、不同坡位(上部、中部、下部)耕层土壤水分特征曲线,并以Van Genuchten(VG)模型拟合该曲线,通过VG模型参数分析比较横坡耕作和顺坡垄作耕作后不同坡位土壤持水特点及其影响因素。
      结果  红壤坡耕地耕层不同坡位土壤与0 ~ 1000 kPa水吸力对应的体积含水率为 0.36 ~ 0.66 cm3 cm−3,VG模型能够较好地表达两者间数量关系。顺坡垄作上部、中部和下部坡位耕层土壤VG模型参数饱和含水率θs分别为0.59、0.59和0.65 cm3 cm−3,残余含水率θr为0.37、0.38和0.41 cm3 cm−3且随着坡位降低而增大;横坡垄作上部、中部和下部坡位耕层土壤VG模型参数饱和含水率θs分别为0.58、0.56和0.59 cm3 cm−3,残余含水率θr为0.37、0.35和0.38 cm3 cm−3且随坡位降低呈先减小、再增加趋势变化。VG模型参数dn均为0.11和0.92,随耕作方向、坡位变化不明显。
      结论  总孔隙度和砂粒含量为影响不同垄作方向红壤耕层理化性质的主导因素。顺坡垄作上部和中部坡位耕层土壤持水能力不及下部坡位土壤,但就同一坡位比较,横坡耕层土壤的释水能力优于顺坡耕作,说明横坡耕作可改善土壤供水能力。

     

    Abstract:
      Objective  Investigating the influence of horizontal ridge and vertical ridges on water characteristics curve of different slope positions would provide a basis for choosing direction of ridge tillage of red sloping farmland.
      Method  The soil moisture characteristic curve of tillage layer in different slope positions (upper, middle, and lower) of two ridge directions were measured by pressure membrane instrument and simulated by Van Genuchten (VG) model. Water retention characteristics and influencing factors of different slope positions of red soil after horizontal ridge and vertical ridge were analyzed and compared by VG model parameters.
      Result  The results showed that the volume moisture contents of tillage layer of different slope positions of red soil corresponding 0 to 1000 kPa water suction were 0.36 to 0.66 cm3 cm−3, and the VG model could better express the quantitative relationship between them. The saturation moisture contents (θs) of upper, middle and lower slopes position of the VG model parameters of vertical ridge were 0.59, 0.59 and 0.65 cm3 cm−3, respectively, and the residual water contents (θr) of them were 0.37, 0.38 and 0.41 cm3 cm−3, respectively. They increased as the slope positions decreased. Saturation moisture contents (θs) of upper, middle and lower slopes position of the VG model parameters of horizontal ridges were 0.58, 0.56 and 0.59 cm3 cm−3, respectively, and residual water contents (θr) were 0.37, 0.35 and 0.38 cm3 cm−3, respectively. The trend of them decreased with the slope positions at first, then increased. VG model parameters d, n were 0.11 and 0.92. With changes of ridge direction and slope position, the changes of d and n were not obvious.
      Conclusion  The results of the principal component analysis showed that total porosity and sand grain content were the leading factors affecting the physical and chemical properties of tillage layer of red soil. The water retention capacities of the upper and middle slope position of tillage layers of vertical ridge were not as good as those of the lower slope position, while the water retention capacities of the upper, central and lower slope position of the horizontal ridge were little difference. The water release capacity of the horizontal ridge of tillage layer was better than that of vertical ridge compared with the same slope position, indicating that the horizontal ridge could improve the soil water supply capacity.

     

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