查询词典 properties of soil
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Phase 1 started with field pea followed by spring wheat whereas phase 2 started with spring wheat followed by field pea.The objectives of this thesis are:1 to quantitatively analyze effects of soil chemical,physical and biological properties on soil quality and productivity under different tillage systems and the driving factors for the changes of soil quality under tillage in a long-term,2 to select the best soil quality assessment indicators,and 3 to establish soil quality assessment models that are suitable for the erodible environment of semi-arid region on the Loess Plateau.
通过分析3个轮作周期不同耕作方式下土壤理化性质、生物性质和生产力对土壤质量的影响,阐明长期耕作过程中土壤质量的演变特征及其驱动因子,筛选出适宜于黄土高原半干旱区侵蚀环境下土壤质量评价的代表性指标;并综合前人的研究,结合区域特点,建立适宜于黄土高原半干旱区侵蚀环境的土壤质量评价模型。
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However,the removal of soil noncrystalline aluminum with DCB soultioncaused an obvious decrease of soil SSA.3.The hydroxy aluminum in the interlayer of 1.4nm intergrade mineralhad an important negative effect on the cation exchange capacity ofsoil colloids.Its removal would cause a significant increase in CEC valuesof the soil colloids.4.Free aluminum was the major carrier of phosphate adsorption of soilcolloids.Particularly,the active aluminum had a decisive effect on thecapacity of phosphate adsorption of soil colliods.5.Addition to the effects of other soil constituents on soil surfaceproperties,it was thought that the effect of soil free aluminum,especially active aluminum on soil surface properties,deserved closeattention.
焦磷酸钠、草酸铵、DCB、柠檬酸钠和NaOH提取的土壤铝对提高土壤CECv、AEC、PZC和PZNC起重要作用,尤以活性铝的作用较大。2)用草酸铵处理除去铝后,土壤比表面积变化不大或略有增加;用DCB处理除去土壤铝后,土壤SSA明显降低。3)层间羟基铝对土壤胶体的阳离子交换量有显著负贡献,用柠檬酸钠将之除去后,土壤胶体的阳离子交换量明显增加。4)土壤胶体中的游离铝是土壤胶体吸附磷的主要载体,尤其是其中的活性铝,对土壤胶体的磷吸附能力起决定性作用。5)除其它土壤组分对土壤表面性质的影响外,土壤中的游离铝、尤其是活性铝对土壤有关表面性质的影响,值得引起特别的重视。
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Soil carbon,soil total N,and pH belonged to high and soil total P belonged to medium degree spatial correlation at 60m lag intervals,respectively.However,there were significant differences in ranges of spatial autocorrelation among four soil properties,among which the effective range of soil organic carbon was the highest(261m),followed with soil total N(208m),pH(156m),and soil total P(133m).
在60m步长间隔尺度下,土壤有机碳、全氮和pH有强烈的空间相关性,土壤全磷空间相关性为中等程度。4种土壤养分的空间自相关范围具有明显的差异,有机碳的有效变程最大(为261m),全氮(208m)和pH(156m)次之,全磷的有效变程最小(133m)。
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Application of Time Domain Reflectometer in geotechnical measurements is a relatively new development. It can be used to measure electrical properties of soils that are related to soil physical properties. In addition, TDR has found applications in monitoring ground water level and relative deformation in soil, rock, or structure.
TDR应用於大地工程之量测为一较新的发展,它除了可以量测与土壤基本物理性质息息相关之土壤电学性质,也可应用於地下水位监测及土壤、岩石之变形监测。
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The stochastic finite element method can consider the random variables which are associated with soil properties, changeable loads, geometric conditions. The stochasitic properties of parameters and seismics will affect the interaction between soil and pile and the stochastic method is a trend to analyze the problem of pile-soil dynamic interaction.
参数和地震激励的随机性对土-结构动力相互作用的影响,土与结构动力学参数的不确定性和地震激励的随机性是众所周知的,其对结构响应的影响也是很重要的,对于结构的地震响应有重要影响的土-结构动力相互作用考虑各种随机因素的影响也是必然的发展趋势。
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By and large, research projects undertaken by the Group fall into three categories. The first is geotechnical properties and prevention of geological hazards, with the stress on researches on dynamic properties of marine soil, coast-beach erosion and seabed failure, sediment reformation by benthonic fauna, failure of submarine pipelines, environmental geotechnical techniques, etc. The second is research on pollution and treatment of water and soil, with the stress on researches on ecological effects of exploitation activities in the marine environment, treatment of beach sediment pollution, treatment techniques of sea organism pollution, groundwater PRB treatment technique development, etc. The third is exploration of underground environment and geophysical data processing techniques, with the stress on devising equipment for detecting underground pollution and geological hazards, environmental GIS (Geographical Information System) and related analysis software, etc.
学术团队开展的研究课题大体上分三类:第一类课题是岩土体性质与灾害防治,侧重于海洋土动力特征研究,岸滩侵蚀与海床破坏研究,海洋底栖生物对沉积物改造研究,海底管线失稳研究,环境岩土工程技术研究等;第二类课题是水土污染过程与治理研究,侧重于海洋开发活动的生态环境效应研究,海滩沉积物污染治理研究,海水生物污染治理技术研究,地下水PRB治理技术开发等;第三类课题是地下环境探测技术与软件开发研究,侧重于地下环境污染与灾害探测设备的研制,环境地理信息系统,专业性应用软件的开发等。
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The soil erodibilities are compared and appraised for the majority of the soil types in Ningxia. The method published by D. W. Fryrear et al is adopted to calculate erodible fractions for the soils in Ningxia. The erodibilities of main soil types are compared and analyzed. Spatial distribution of soil erodibilities in the region can be perceived on the Map of Ningxia Soil Erodibility. The map is based on the digitized map of soil types of the all region by means of the geographical information system of Region Manager. Evaluation results show that erodible soils occupy a large portion of the total area of the region.(3) The third task is evaluation of effects of human activities for farming on soil erodibility. Tillage and cultivation can alter soil properties. The paper, based on the discussion on the characteristics of farmland suffering wind erosion in the region, analyzes the contents and intensities of farming disturbing surface soil. Emphasis is paid on the effect of farming on erodibilities of each type of soil.
W Fryrear等人的计算土壤可蚀部分含量的方程,此方程的自变量包括土壤有机质、碳酸钙、沙粒含量、沙粘比,计算了宁夏主要土壤类型表层的可蚀含量,进而比较它们的可蚀性,并以宁夏土壤分布图为底图用地理信息系统建立了宁夏土壤风蚀数据库,完成了宁夏土壤可蚀性图,评价结果显示宁夏地区主要的土壤类型较容易遭受风蚀;(3)农业经营对土壤风蚀的影响及其评价,在分析宁夏农业土壤遭受风蚀特征的基础上,首先讨论了农业活动对土壤理化性质的干扰,评价主要耕作栽培措施对土壤风蚀的影响,选取粗糙度、表面结皮、可蚀颗粒含量、留茬和有效时间为指标,用打分方法作了评价。
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Better numerical prediction of the distributions of shear forces and bend moment within the pile group has also been obtained with the consideration of many stochastic parameters such as the soil properties of sea warf, seismic properties, etc. And then we analyze the dynamic nonlinear seismic pile-soil interaction in sea warf as an example to apply the software of ANSYS to the assessment of the dynamic interaction of soil-structure in the harsh situation of random earthquake. And then we denoted that the soil-pile interaction is too difficult to be expressed in equations because the non-linear interaction between soil and pile.
5桩基由于其本身的优点得以在海洋码头结构中大量的运用,但是海洋码头结构在海洋环境下受多方面的影响,土与桩体的相互作用关系很难清楚的表达,由于影响因素的多样性及复杂性,以及它们与桩基性状之间的非线性和非确定关系,使得关于桩基性状的各种理论解答还不能采用简便的表达式以反映其复杂多变的机理,尤其是难于反映施工及环境因素对桩基性状的影响,而且如何发挥桩基的技术经济效益和如何合理的确定桩的极限承载力,也是一个技术难度很大的问题。
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Consolidation test is a important link of obtaining mechanical properties index of soil and coefficient of compressibility gained through the test is a key data to evaluating the compressibility of soil. Consisting of solid phase and liquid phase of the salty soil is different from the non-salty one. Eutectic salt in soil may exist as liquid phase, solid phase or both of them and these phases can interconvert because it is affected by temperature, Na_2SO_4 content, water content. Especially when temperature drops, Na_2SO_4 will crystallize and expand, namely salt expansion of soil. These particularities make soil sample put in environmental cabinet when consolidation test is going on. So soil sample can be compressed by temperature controlling system under a set temperature.From experiment, the formulae counting coefficient of compressibility of salty soil have been given.
土的固结试验,是取得土的力学性质指标的一个重要环节,因为土的固结试验所取得的压缩系数,对评价土的压缩性是一个关键数据,但由于盐渍土的固相、液相组成和非盐渍土不同,土中易溶盐受温度、含盐量、含水量的影响可以以液相、固相、液相和固相混合形式存在,且它们之间的存在形式可以相互转换,尤其是当温度下降时,硫酸钠便结晶产生体积膨胀,即盐胀,这些特殊性就使得在进行硫酸盐渍土的固结实验时,须将土样放置在环境箱中,通过温度控制系统使土样在设定的温度下受压产生变形。
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Statistic analysis showed that soil temperature as the driving factor to the diurnal variation of soil respiration. Soil temperature and soil moisture were the dominant environmental factors affecting the seasonal variation of soil respiration and explained 87% of its variability. LAI and root biomass were positively related to soil respiration rate, indicating that biotic factors also affected the seasonal variation of soil respiration. However, soil properties such as soil organic content, total nitrogen content, and C/N ratio had poor correlations with soil respiration. Top-dressing nitrogen fertilizer increased soil respiration significantly.
统计分析表明:土壤温度是玉米生态系统土壤呼吸日变化的驱动因素;土壤温度和土壤水分是影响土壤呼吸季节变化的关键因素,二者可以解释玉米生长季土壤呼吸时间变异的87%;LAI和根系生物量与土壤呼吸速率呈正相关,说明生物因子对土壤呼吸季节变化也有影响;土壤有机质、全氮和碳氮比等土壤理化特性与土壤呼吸速率的关系较弱;玉米生长季追施氮肥明显促进土壤呼吸速率。
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Do you know, i need you to come back
你知道吗,我需要你回来
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Yang yinshu、Wang xiangsheng、Li decang,The first discovery of haemaphysalis conicinna.
1〕 杨银书,王祥生,李德昌。安徽省首次发现嗜群血蜱。
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Chapter Three: Type classification of DE structure in Sino-Tibetan languages.
第三章汉藏语&的&字结构的类型划分。