玉米茎秆汁液对土壤的减水减沙效益及其机理

为研究土壤改良剂玉米茎秆汁液对中国西部地区水土流失的影响和机理,该文通过室内土壤理化性质测定和人工模拟降雨试验,研究了地表施加玉米茎秆汁液对土壤团聚体的平均重量直径、土壤有机质质量分数和土壤减水减沙效益的影响。试验以未施加任何玉米茎秆汁液的黄土坡面为对照,设计单位面积玉米茎秆汁液施加量1 041.7 mL/m2,施加汁液体积分数25%和50%,降雨强度为50 mm/h,研究玉米茎秆汁液施加对土壤减水减沙的影响。结果表明,玉米茎秆汁液的施加可以增加土壤有机质的含量,提高土壤团聚体的平均重量直径,降低产流产沙速率。对照、体积分数25%和50%汁液施加下的土壤团聚体平均重量直径分别为0.18、0.46和0.51 mm,土壤有机质质量分数分别为5.70%、6.75%和7.17%。较对照,体积分数25%和50%汁液施加下,土壤的减水效益分别为45.81%和48.34%,减沙效益分别为65.00%和75.47%。玉米茎秆汁液的减水减沙效益随时间的推移而降低,月均减水、减沙效益降低量约为1.25%和1.41%,研究中施加体积分数25%和50%汁液的土壤减水减沙效益约可持续3和4.5 a。综上,玉米茎秆汁液作为土壤改良剂在施加量为1 041.7 mL/m2时,茎秆汁液与水的体积比为1:1时,效果较好。该研究可以为将玉米茎秆汁液作为土壤改良剂用于土壤侵蚀的防治提供施放参考。     

武夷山土壤形成特点与系统分类

选取武夷山土壤垂直带中 6个代表性剖面 ,研究了土壤的形成条件和特点 ;按照《中国土壤系统分类 (修订方案 )》 ,鉴定了诊断层和诊断特性 ,检索了土壤系统分类名称 ;随海拔由低到高 ,依次为湿润富铁土—湿润淋溶土—常湿淋溶土—常湿雏形土等亚纲 ;并与发生学分类、美国土壤系统分类 (USST)以及世界土壤资源参比基础 (WRB)等不同分类系统中的土壤类别归属作了参比     

Use of poultry manure and plant cultivation for the reclamation of burnt soils

Annual (Pisum sativum L. and Vicia sativa L.) and perennial (Trifolium repens L. and Lotus corniculatus L.) leguminous species were grown in pots containing samples from the ash layers of two Cambisols under Pinus sylvestris L., which has been affected by high-intensity wildfires 3 and 15 days before the sampling. The gramineous Lolium perenne L. was cultivated as a second plant after Trifolium and Lotus harvesting. Three treatments were compared: soils without fertilization and soils fertilized with two doses of poultry manure (1 and 2 g total N kg^-1 dry soil). The aim of the work was to study the capacity of the ash layer to sustain vegetation and the influence of plants and organic manure on the recovery of vegetation cover, ash layer fixation and soil structure formation to avoid erosion. The ash samples were able to sustain vegetation without fertilization. The organic manure increased the yields of all the plants tested, the lower dose being the optimal for the first crop whereas the higher dose was beneficial for the second crop. The annual legumes grew very quickly. The mixture of Trifolium and Lotus seemed very suitable for reclamation of soil degraded by wildfires because Trifolium produced more phytomass than Lotus in the first growing stages whereas the development of Lotus was higher in the later growing stages. Ash layer conditions did not inhibit nodulation, which was, however, stimulated by the organic manure, particularly in the case of Lotus. Lolium after perennial legumes was the best plant combination because it produced the highest phytomass, particularly root phytomass, and thus improved vegetation cover and ash layer fixation. All the plants tested improved the formation of soil aggregates, particularly the combination of perennial legumes and Lolium. However, wet aggregate stability was higher when plants were grown on soils fertilized with poultry manure than when plants were cropped on unmanured soils, which points to the favourable influence of the organic manure on soil aggregation.     

皖南紫红色砂石岩上发育土壤的系统分类研究

对皖南不同时期紫红色砂石岩上发育的8个土壤剖面,按中国土壤系统分类体系,进行鉴别、检索、分类定名。阐述发生分类紫色土的2个亚类级土壤类型在中国土壤系统分类中归为3个土纲,即均腐土、雏形土和新成土;3个亚纲,即湿润均腐土、湿润雏形土和正常新成土;4个土类和6个亚类。提出按中国土壤系统分类的紫色土分类系统;并与美国土壤系统分类、国际土壤分类参比基础进行了参比。讨论了皖南紫红色砂石岩上发育为均腐土的成土环境条件,同时对发生分类紫色土在中国土壤系统分类类别检索提出修订建议。     

集中排水甘蔗地酸性硫酸盐土壤酸化的减缓

Recent research results suggest that acidification of acid sulfate soils may be inhibited in well-drained estuarine floodplains in eastern Australia by the absence of natural creek levees,The lack of natural levees has allowed the inuudation of the land by regular tidal flooding prior to the construction of flood mitigation work.Such physiographical conditions prevent the development of pre-draingae pyrite-derived soil acidifica-tion that possibly occurred at many levee-protected sites in eastern Australian estuarine floodplains during extremely dry spells.Pre-drainage acidification is considered as an important condition for accumulation of soluble Fe and consequently,the creation of favourable environments for catalysed pyrite oxidation.Under current intensively drained onditions,the acid materials produced by ongoing pyrite oxidation can be rapidly removed from soil pore water by lateral leaching and acid buffering,resulting in low concentrations of soluble Fe in the pyritic layer,which could reduce the rate of pyrite oxidation.     

Effect of low-molecular-weight organic acids on Cl- adsorption by variable charge soils

Low-molecular-weight (LMW) organic acids exist widely in soils and have been implicated in many soil processes.The objective of the present paper was to evaluate effect of two LMW organic acids, citric acid and oxalic acid, on Cl^- adsorption by three variable charge soils, a latosol, a lateritic red soil and a red soil, using a batch method. The results showed that the presence of citric acid and oxalic acid led to a decrease in Cl- adsorption with larger decreases for citric acid. Among the different soils Cl- adsorption in the lateritic red soil and the red soil was more affected by both the LMW organic acids than that in the latosol.     

土壤环境质量指导值与标准研究 Ⅱ.污染土壤的健康风险评估

快速城市化进程与工业发展，使得土壤污染日益严重。污染物进入土壤后，经水、气、生物等介质传输，通过饮水、呼吸、饮食、皮肤吸收等途径引起人体暴露，带来健康风险。污染土壤健康风险评估是制定土壤环境质量标准的基础，是一项新的环境管理技术与手段。我国污染土壤的健康风险评估还非常欠缺，为了推动其发展，本文讨论了其研究进展、方法、存在问题与发展趋势。当前，还缺乏准确定量的风险表征方法，评估过程中还具有较大不确定性。污染土壤的健康风险评估正在向多介质、多途径以及多种污染物暴露的方向发展，模型模拟的方法将会得到更多的应用。为了建立准确定量风险评估方法，在未来研究中需要加强对风险评估相关机理研究。这包括污染物的迁移传输规律、污染物的剂量一效应关系和人群生活方式等。     

用稀悬液Wien效应测量法来研究重金属离子与水稻土的相互作用

Interactions of three heavy metal ions, Cu²⁺, Cd²⁺, and Pb²⁺, and, for comparison, Na⁺ with electrodialytic clay fractions (less than 2 μm in diameter) of four paddy soils as well as a yellow-brown soil as a control soil were evaluated based on measurements of the Wien effect in dilute suspensions with a clay concentration of 10 g kg^?1 in four nitrate solutions of 2 × 10^?4/z mol L^?1, where z is the cation valence, and a nitric acid solution of 3 × 10^?5 mol L^?1. Field strengths ranging from 15 to 230 kV cm^?1 were applied for measuring the electrical conductivities (ECs) of the suspensions. The mean free binding energies between the various cations and all of the soils determined from exchange equilibrium increased in the order: Na⁺ < Cd²⁺ < Cu²⁺ < Pb²⁺. In general, the ECs of the suspensions in the sodium nitrate solution were smaller than those of the suspensions in the heavy metal solutions because of the lower electrophoretic mobility of sodium compared to the divalent cations. In terms of relative electrical conductivity-field strength relationships, relative electrical conductivity (REC) of suspensions containing various cations at field strengths larger than about 50 kV cm^?1 were in the descending order: Na⁺ > Cu²⁺ > Cd²⁺ > Pb²⁺ for all tested soils. A characteristic parameter of the REC-field strength curves, ΔREC₂₀₀, REC at a field strength of 200 kV cm^?1 minus that at the local minimum of the concave segment of the REC-field strength curves, characterized the strength of adsorption of the cations stripped off by the applied strong electrical field, and for all soils the values of ΔREC₂₀₀ were generally in the order: Na⁺ < Cu²⁺ ≤ Cd²⁺ ≤ Pb²⁺.     

The causes of piping in a set of abandoned agricultural terraces in southeast Spain

This study aims to identify some of the factors contributing to the piping process in abandoned terraces in seven sites located in the Murcia Region (southeast Spain). The local landscape has the appearance of badland geomorphology, possessing deep valleys which until the 1970s were terraced and cultivated. The terraces have now been abandoned to the piping process. The research focuses on the relationship between the size and position of pipes and the physical and geochemistry properties of the local highly dispersive marl lithology; and the extent to which the reworking of the materials for terrace cultivation has exacerbated piping erosion.Morphologically, the terracing in the stream beds has resulted in a series of gentle benches separated by steeper risers with variable ‘drop’, (riser height). A series of flat infiltration surfaces result, and because the resculpting produces a reduced bulk density infill with enhanced throughflow, infiltrating water is forced along steep hydraulic gradients to a low outfall at the base of the riser.Paralleling studies of land levelling and terrace abandonment in similar materials elsewhere, piping in the study area is shown to be closely related to the physical and chemical characteristics of the materials its sodicity and dispersive character. Considerable differences in structure, texture, mineralogical composition and material's surface crust and subsoil geochemical properties emerged from ‘site signature’ plots, and these results suggest that agricultural processes affect the dispersive character of the crust materials, presumably because agricultural activity increases the buffering effect of organic acids on the dispersed clay. This is supported by the observation that on the one site that was levelled but not used for agriculture, a stable organically-distinct crust like the abandoned agricultural sites has not formed. The changes to the material's aggregate stability and bulk density properties when terracing occurs is examined, but insufficient evidence is available from the data collected to unpick the causes of aggregate stability changes in the study plots. The way in which differences between crust and subsoil enhance infiltration is discussed, and the role of the terrace ‘drop’ in influencing hydraulic gradients and pipe development is illustrated. A possible index to describe the relationship between evacuated material volumes and the controlling parameters discussed above is tested.It is concluded that terracing which is intended as a conservation practice has, in dispersive materials, actually enhanced piping, leading to the abandonment of farming.     

Differences in common bean rhizobial populations associated with soil tillage management in southern Brazil

Progressive adoption of no-tillage (NT) agriculture in the tropics is finally reversing physical, chemical, and biological erosion of soil and in Brazil, an estimated 19 Mha are now devoted to NT. Common bean (Phaseolus vulgaris L.) is a main component of Brazilian agriculture, and enhancement of yields has been achieved under NT as a result of mitigation of environmental stresses, resulting in higher N₂ fixation. However, the effects of NT on rhizobial diversity are poorly understood. This study evaluated rhizobial diversity in soils planted to common bean under NT or conventional tillage (CT) systems that were compared with natural grassland used for grazing, in the State of Santa Catarina, southern Brazil. Genetic diversity was assessed by the amplification of the DNA by PCR with specific primers (BOX-PCR) and by RFLP-PCR analyses of the 16S rDNA region. A high level of diversity was observed among strains from all three systems, such that the similarity in the clustering analysis of BOX-PCR products ranged from 36% under natural grassland to only 23% for CT strains. High polymorphism was confirmed in the RFLP-PCR analysis; forty-seven different profiles were obtained, none sharing high similarity with the profiles of reference species of common bean rhizobia. These results indicate that other tropical rhizobial species remain to be described. Genetic diversity was higher among the NT than the CT rhizobial strains, especially when the RFLP-PCR profiles were considered. Genetic diversity in the natural grassland was lower than in the cropped systems, possibly due to absence of the host plant and stubble burning in winter. Average yields in the area under NT (e.g. common bean, approximately 1500 kg ha⁻¹) have been about 30% higher than under CT, therefore high rhizobial diversity may be a parameter indicative of superior soil quality.