首页> 外文期刊>Geoderma: An International Journal of Soil Science >Effects of three morphometric features of roots on soil water flow behavior in three sites in China
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Effects of three morphometric features of roots on soil water flow behavior in three sites in China

机译:根系三种形态学特征对我国三个地点土壤水流行为的影响

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摘要

Soil physical properties, infiltrability, and water flow behavior are closely associated with root morphology. In this study, dye tracer experiments were conducted in the field to assess the effects of roots with various morphometric features on soil water flow behavior and soil infiltrability. Preferential flow is the dominant type of water flow in the three study sites (Minqin, Dongtai, and Mengla). The presence of roots caused noncapillary porosity and saturated hydraulic conductivity to increase by 26% and 252% in the Minqin, 92% and 93% in the Dongtai, and 234% and 96% in the Mengla, respectively, relative to that in in soils without roots. The various morphometric features of roots affect water flow behavior in soil. The fibrous roots of maize induced water to flow and distribute evenly throughout the plough layer of the study site in Minqin. Furrows and ridges in this site exhibited different soil physical and hydrological properties. Furrows could store higher amounts of water than ridges, thereby increasing the likelihood of water absorption by plants. In Dongtai, ponding and surface runoff occurred when water infiltration was inhibited by the mud layer, which exhibited a high soil bulk density value of 1.43 g cm(-3) and a low saturated hydraulic conductivity value of 1.67 x 10(-5) CM s(-1). These phenomena were not observed in plots the smooth roots of Spartina alternifiora penetrated the mud layer. In this site, preferential flow and lateral flow, which is triggered by the sandy loam layer, are important for water discharge from the beach to the ocean. In Mengla, water flowed evenly on hard soil, which exhibited a high bulk density value of 1.43 g cm(-3). The fine roots of rubber could guide water infiltration into deep soil layers (73.54 cm), thereby redistributing water to the root zones of rubber trees. Therefore, our findings indicated that water infiltration behavior, which is crucial for water distribution, is affected by the various morphometric features of roots.
机译:土壤物理性质,浸泡和水流动行为与根形态密切相关。在该研究中,在现场进行了染料示踪实验,以评估根部水流动行为和土壤浸泡各种形态学特征的根源的影响。优惠流动是三个研究网站(Minqin,Dongtai和Mengla)中的主要水流类型。根部的存在导致非足孔隙率和饱和液压导电率分别在Minqin,92%和93%中增加了26%和252%,分别相对于土壤中的蒙加拉分别为234%和96%没有根。根系各种形态学特征影响土壤中的水流动。玉米诱导水的纤维根流动流动,在Minqin的研究部位的整个犁过层中均匀分布。该网站的沟和脊表现出不同的土壤物理和水文特性。沟槽可以存储比脊更高的水,从而增加了植物吸水的可能性。在Dongtai,泥浆层抑制水渗透时发生了池塘和表面径流,该泥浆层抑制了1.43g cm(-3)的低土堆积密度值和低饱和液压电导率值1.67×10( - 5)cm s(-1)。在绘制Spartina交别的平滑根渗透到泥层中,没有观察到这些现象。在该网站中,由桑迪壤土层触发的优先流量和横向流动对于从海滩到海洋的水排放是重要的。在Mengla,水在硬土上均匀流动,其展示了1.43g cm(-3)的高堆积密度值。橡胶的细根可以将水浸润引导到深土层(73.54cm)中,从而将水重新分配到橡胶树的根区域。因此,我们的研究结果表明,对水分布至关重要的水渗透行为受根源各种形态学特征的影响。

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  • 作者单位

    Chinese Acad Sci Key Lab Trop Forest Ecol Xishuangbanna Trop Bot Garden Menglun 666303 Yunnan Peoples R China;

    Chinese Acad Sci Key Lab Trop Forest Ecol Xishuangbanna Trop Bot Garden Menglun 666303 Yunnan Peoples R China;

    Chinese Acad Sci Key Lab Trop Forest Ecol Xishuangbanna Trop Bot Garden Menglun 666303 Yunnan Peoples R China;

    Chinese Acad Sci Key Lab Trop Forest Ecol Xishuangbanna Trop Bot Garden Menglun 666303 Yunnan Peoples R China;

    Chinese Acad Sci Northwest Inst Ecoenvironm &

    Resources State Key Lab Frozen Soil Engn Lanzhou 730000 Gansu Peoples R China;

    Guizhou Univ Coll Anim Sci Guiyang 550025 Guizhou Peoples R China;

    Hohai Univ State Key Lab Hydrol Water Resources &

    Hydraul En Nanjing 210098 Jiangsu Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 土壤学;
  • 关键词

    Preferential flow; Matrix flow; Rhizopore; Dye tracer; Capillary force;

    机译:优先流动;矩阵流动;Rhizopore;染料示踪剂;毛细管力;

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