基于统一硬化参量的海洋K0固结土动力本构模型

为方便海洋工程中桩土相互作用计算,根据海洋K₀固结土体特性,对现有相关土体本构模型进行简化。在修正剑桥模型的基础上,基于热力学理论,选用耗散功作为硬化参量,结合原状土体的固结属性,推导了适用于黏土与砂土的统一硬化模型。在此基础上,通过采用旋转硬化与等向硬化相结合的硬化理论来表征K₀固结土在循环荷载作用下的硬化规律,同时引入屈服面收缩参数Θ来描述循环荷载加载过程中土体屈服面的演化特性,进而建立了循环荷载下海洋K₀固结土体统一硬化模型。为验证本文提出的本构模型的合理性,开展了2个案例的对比研究,研究结果表明:新提出的统一硬化模型的计算值与实测值吻合,选用的计算参数少且物理意义明确。     

Comparison of soil moisture at different depths for drought monitoring based on improved soil moisture anomaly percentage index

To better understand the characteristics and mechanisms of droughts at different drought stages, this study selected the Xiangjiang River Basin in China as the study area, and evaluated soil moisture (SM) at different depths for drought monitoring, through SM data simulated with the variable infiltration capacity (VIC) model. To solve the problem of unreasonable drought/wetness classifications based on the soil moisture anomaly percentage index (SMAPI), an improved soil moisture anomaly percentage index (ISMAPI) was developed by introducing the Box–Cox transformation. The drought/wetness frequency generated by ISMAPI demonstrated preferable spatial comparability in comparison with those from SMAPI. The lag time of ISMAPI relative to the standardized precipitation evapotranspiration index was closely related to soil depth, and was characterized by a fast response in shallow soil layers and a relatively slow response in deep soil layers. SM in shallow soil layers provided a measure for monitoring short-term droughts, whereas SM in deep soil layers provided a better measure for long-term persistent drought events. Furthermore, the occurrence and mitigation time of drought events identified by SM in deep soil layers usually lagged behind that identified by SM in shallow soil layers. Compared with deep SM, SM in shallow soil layers responded faster to meteorological anomalies, thereby resulting in shorter periods of SM persistence in shallow soil layers than in deep soil layers. This can explain the differences of SM at different depths in drought monitoring.     

用仪器中子活化分析法检验环境土壤标样的均匀度

近年来,国际上标准参考物质的种类与数量急剧增加,一些重要的领域,象地球化学、环境科学、生物学等都有了相应的SRM。国内研制SRM的工作也十分活跃。 标准样品必须均匀,故在分析定值和样品发行前,需要先作均匀性检验。由于均匀性是一个相对的概念,它与各个元素在SRM中的分布紧密相关。取样量直接影响均匀性的好坏。因此,当给出SRM中某元素的均匀性数值时,必须注明相应的取样量。由于仪器中子活化分析法(INAA)具有灵敏度高、不破坏试样、且可同时测定多种元素等特点,因此可在较小的取样量情况下,实现对SRM中多种痕量元素的均匀性检验。     

小型预制桩基础承载特性数值模拟研究

本文建立硬化土本构模型,针对江苏省软土地区的土质条件选取数值计算参数,通过PLAXIS 2D软件对小型预制桩在的单桩水平受荷及竖向受荷进行数值模拟,得到桩身弯矩沿桩长的分布以及荷载-位移曲线,分析小型预制桩基础桩身弯矩的分布特点,并探求其在水平及竖向荷载作用下的承载特性,进而能够为小型预制桩基础工程设计以及计算方面提供一定的参考依据。     

加芯搅拌桩芯桩定位限垂技术的研发与应用

为控制水泥土加芯搅拌桩的芯桩贯入质量,研发了一种基于芯桩定位导向架的定位限垂挑臂装置,并通过采用不同材质、不同尺寸的方法,反复摸索、实施,分析得出了芯桩定位导向架的定位限垂挑臂装置的最优方案。同时,通过运用数据比对、图表说明的方法,有效验证了加芯搅拌桩芯桩定位限垂挑臂装置对于现场施工的重要作用。在新疆地区23450 根加芯搅拌桩工程中进行首次应用,实践表明研发的定位限垂技术可有效控制芯桩贯入的定位和垂直度,提高施工效率。该定位限垂技术经济效益良好,可为今后新疆地区特殊软基处理以及加芯搅拌桩施工提供参考价值。     

腐解稻草DOM提取液洗脱六价铬污染土壤试验研究

工矿企业产生的铬渣、含铬废水由于管理不善导致土壤铬污染严重,迫切需要寻求低成本铬污染土壤修复技术。提出腐解稻草中溶解性有机质（Dissolved Organic Matter, DOM）提取液洗脱铬污染土壤的技术,通过实验室模拟试验,以2种铬污染土壤（总铬含量为分别为121.54、941.90 mg/kg,六价铬含量分别为119.90、856.90 mg/kg）为研究目标,采用振荡淋洗法考察了固液比、淋洗时间、淋洗次数等因素对土壤中总铬、六价铬洗脱效果的影响,并探讨了淋洗前后铬形态变化及淋洗后土壤残留六价铬的持续钝化能力。研究结果表明：稻草经35 d腐解后的DOM提取液洗脱土壤中铬效果最佳,确定为最佳淋洗剂;固液比1：15、淋洗4h/次、淋洗2次为最佳淋洗工艺条件,该条件下,2种铬污染土壤总铬分别洗脱了47.79%、85.92%,六价铬含量分别削减了51.76%、95.09%;DOM提取液呈弱碱性,包含大量羧基、羟基及酚类物质,对水溶态、弱酸提取态和残渣态铬有较好的洗脱效果,有效降低了土壤环境风险,且能持续钝化淋洗后土壤中残余的六价铬。     

区域土壤腐蚀试验数据分布特征研究——Ⅰ 概率分布特征表述

以塔里木和大港油田区域土壤腐蚀试验数据为例，论 证了区域腐蚀试验数据整体概率分布符合正态随机函数、其极大值数据符合Gumbel极值函数 .根据分布参数可以计算区内不同腐蚀性土壤比例、可能存在最大土壤腐蚀性和出现的概率 等工程信息.     

中原油田-曲阜-济南天然气管道工程沿线土壤腐蚀性评价

依据SY／T0007—1999《钢质管道及储罐腐蚀控制工程设计规范》对中原油田-曲阜-济南天然气管道工程沿线土壤进行了腐蚀评价，指出该管道沿线土壤以中强性腐蚀为主，文章对土壤腐蚀评价过程进行了较详细的介绍。     

土壤中阴离子对碳钢腐蚀的影响

应用弱极化曲线技术和交流阻抗谱研究了土壤中C1-、SO4^2-、CO3^2-、NO3-离子对碳钢腐蚀的影响。结果表明：阴离子对碳钢腐蚀的影响是显著的。当土壤中分别添加Cl-、CO3^2-、NO3-离子时，随着阴离子含量的增大，碳钢的腐蚀速率增大，在某一离子含量时，腐蚀速率达到最大，然后腐蚀速率随着离子含量的增加而减小。在含SO4^2-离子的土壤中随着SO4^2-离子含量的增大，土壤中碳钢的腐蚀速率增大。在有四种阴离子土壤中，阻抗谱均为单容抗弧，且大都在低频区出现扩散弧。     

Simulation of nitrogen dynamics and biomass production in winter wheat using the Danish simulation model DAISY

A dynamic simulation model for the soil plant system is described. The model includes a number of main modules, viz., a hydrological model including a submodel for soil water dynamics, a soil temperature model, a soil nitrogen model including a submodel for soil organic matter dynamics, and a crop model including a submodel for nitrogen uptake. The soil part of the model has a one-dimensional vertical structure. The soil profile is divided into layers on the basis of physical and chemical soil characteristics. The simulation model was used to simulate soil nitrogen dynamics and biomass production in winter wheat grown at two locations at various levels of nitrogen fertilization. The simulated results were compared to experimental data including concentration of inorganic nitrogen in soil, crop yield, and nitrogen accumulated in the aboveground part of the crop. Based on this validation it is concluded that the overall performance of the model is satisfactory although some minor adjustments of the model may prove to be necessary.