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首页> 外文期刊>Soil & Tillage Research >Soil solution composition affects microstructure of tropical saline alluvial soils in semi-arid environment
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Soil solution composition affects microstructure of tropical saline alluvial soils in semi-arid environment

机译:土壤溶液组成影响半干旱环境中热带盐水冲积土的微观结构

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摘要

The remediation of soils stressed by salinity improves soil quality for food production. However, information on how remediation techniques affect microstructural stability/elasticity and resistance is lacking. Hence, the objective of this study was to characterize the microstructure of saline alluvial soils from a semi-arid environment, and to evaluate how the techniques of leaching soil and Na+ substitution by other cations affect the microstructure strength and elasticity evaluated by rheological techniques. Homogenized soil of sixteen horizons of four salinized soil profiles (an Abruptic Solonetz, a Eutric Gleysol, and two Hypereutric Planosols) were collected in Northeast of Brazil. Each horizon was analyzed separately in a completely randomized design, with three replications. The treatments corresponded to soils saturated with 1 x 10(-4) mol m(-3) of KCl (+K), CaCl2 (+Ca) or MgCl2 (+Mg), leaching of salts (LS) by successive leaching with alcohol 60%, and untreated soil (control). The soils were submitted to an amplitude sweep test with controlled strain in a compact modular rheometer. The obtained variables were strain and stress at the end of the linear viscoelastic interval (LVR) (gamma(LVR) and tau(LVR), respectively), strain (gamma(YP)) and stress (G'(YP)) at the yield point, shear stress (tau(max)), and integral Z (Iz). The rheological properties varied greatly between the horizons of the same soil profile. The LS increased. LVR compared to control, while the saturation with cations caused reduction in gamma(LVR), especially in soils of higher clay content. The saturation with saline solution increased gamma(YP) and Iz, with greater effect in + K treatment. Both leaching of salts and cation saturation increased soil shear strength at the end of the LVR and at the yield point. Leaching of salts caused destabilization of soil microstructure, which is an important finding that needs to be addressed by measures accompanying remediation of salinized soils to maintain soil physical quality.
机译:用盐度强调的土壤的修复可以提高食品生产土壤质量。然而,有关修复技术如何影响微观结构稳定性/弹性和阻力的信息。因此,本研究的目的是表征来自半干旱环境的盐水冲积土的微观结构,并评估其他阳离子的浸出土壤和NA +替代的技术如何影响通过流变技术评价的微观结构强度和弹性。在巴西东北部收集了四个盐渍土曲线的十六个视野(突然Solonetz,eFutric Gleysol和两个过度r rsolsols)的均质土壤。在完全随机设计中分别分别分析各种地域,有三种复制。该处理对应于饱和1×10(-4)摩尔M(-3)KCl(+ K),CaCl 2(+ Ca)或MgCl 2(+ Mg)的土壤,通过连续用醇浸出盐(LS)浸出60%和未经处理的土壤(对照)。将土壤提交到具有控制应变的振幅扫描测试,在紧凑的模块化流变仪中。所得变量在线性粘弹性间隔(LVR)(LVR)的末端(γ(LVR)和TAU(LVR)的末端进行应变和应力,菌株(γ(γ))和应力(G'(G'(YP))屈服点,剪切应力(TAU(MAX))和积分Z(IZ)。流变性质在相同土壤剖面的视野之间变化。 LS增加。 LVR与对照相比,阳离子饱和导致γ(LVR)降低,尤其是粘土含量的土壤。用盐水溶液饱和γ(yp)和Iz的饱和度,+ k治疗方面具有更大的效果。盐酸盐和阳离子饱和度的浸出量增加了LVR末端的土壤剪切强度和屈服点。盐的浸出造成了土壤微观结构的破坏性,这是一种重要的发现,需要通过伴随盐渍土的修复来保持土壤体质的措施。

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