滩槽流量分别演算法进行汾河下游河段洪水预报

汾河下游柴庄以下河段由于受人为和处在然等多种因素影响,河道发生持续淤积,过水能力大幅度降低,使河道行洪特点发生很大变化,正常洪水预报方法失效。     

Geochemical demobilization of metallic pollutants in solid waste—implications for arsenic in waterworks sludges

During stabilization or demobilization of contaminants in solid waste materials, different approaches can be taken, which also can be combined: (1) sufficient long-term buffer capacity can be provided, according to the environmental conditions; (2) permeability for dissolved contaminants can be reduced by secondary mineral precipitations or by soft gels injected into the pore space of the waste body; and (3) new formations of ‘reservoir minerals' can incorporate potential pollutants in their internal structure. Emphasizing the geochemical engineering approach, two examples are presented from the field of water management, both focussing on the demobilization of arsenic species. The first example (after Driehaus, W., 1994. Arsenentfernung mit Mangandioxid und Eisenhydroxid in der Trinkwasseraufbereitung. Vol. 133, Ser. 15, VDI-Reports, Düsseldorf, 117 pp.) relates to the problems during purification of arsenic-rich raw water, suggesting the potential application of iron and manganese oxide minerals as oxidizing agents and mineral lattice structures for the elimination of arsenic. In the second example, contaminated sludges from water treatment plants were investigated for their leaching characteristics and long-term stability. A pH-stat test procedure was used to assess the leaching characteristics of metals at typical pH values. Due to the presence of iron and manganese oxides pentavalent arsenic is protected against conversion into the mobile trivalent form at neutral to low pH. Experimental data suggest that co-disposal with reducing organic matter and alkaline stabilization material or wastes could negatively influence the binding properties and, therefore, should be avoided.     

Charts for probabilistic design of strip footings in cohesionless soils

Design charts that enable quick determination of the probability distribution parameters related to the ultimate bearing capacity of shallow foundations resting on (c = 0) soils are developed. These charts are intended to assist foundation designers and analysts in studying the reliability of structures as related to the capacity of the foundation system. The approach presented herein provides a more reliable alternative to foundation design and analysis than the current conventional design procedure which employs the assumption of an appropriate factor-of-safety. © Rapid Science Ltd. 1998     

地电化学提取法的理论与实验研究

根据离子溶液电化学的基本性质和稳定电流场的基本理论,通过理论计算和物理模拟实验,指出：离子在外电场作用下,由所在地点迁移至接收电极所需时间与多种因素有关,当外界条件一定时,加大供电电流强度可减少接收时间;离子淌度值很小,由实测时量曲线计算出的ｕｉ值,一般不超过几个ｃｍ２·ｈ－１·Ｖ－１单位,因此欲提取深部离子,即使在最有利条件下也是非常困难的;由不同供电电流强度测出的时量曲线,计算得到的淌度值是相等的,因此改变供电电流强度并不能改变离子淌度值,但当围岩介质的颗粒度较大时,可使离子淌度值变大;离子的迁移质量与供电电量Ｑ＝Ｉ·ｔ成正比,因此在供电电流强度不变的条件下,采用间断供电方式可取得与连续供电相同的结果;通过浅部已存在的离子晕,用电提取法可以发现深部隐伏矿体。     

上海某超高层建筑采用静压桩工艺取得成功引起的思考

通过高压静压桩取得成功的实例介绍,表明在大能量压桩机日益发展的有利条件下,配以有效的防挤措施,在上海闹市区有可能重新大量使用质量可靠又经济的预制砼桩。     

多分支承力盘桩的特性分析

从理论和实践说明多分支承力盘桩是一种经济效益好，承载力高的新型桩基。     

MASINGA RESERVOIR IN KENYA：SEDIMENT DISCHARGE AND IMPLICATIONS FOR ITS CAPACITY

ＭＡＳＩＮＧＡＲＥＳＥＲＶＯＩＲＩＮＫＥＮＹＡ：ＳＥＤＩＭＥＮＴＤＩＳＣＨＡＲＧＥＡＮＤＩＭＰＬＩＣＡＴＩＯＮＳＦＯＲＩＴＳＣＡＰＡＣＩＴＹ￥Ｆ．Ａ．Ｏ．Ｏｔｉｅｎｏ（ＳｅｎｉｏｒＬｅｃｔｕｒｅｒｉｎＣｉｖｉｌＥｎｇｉｎｅｅｒｉｎｇ，Ｕｎｉｖｅｒｓｉ...     

碎石桩复合地基承力性状有限元分析

本文通过对碎石桩复合地基的简化，采用有限元方法分析了复合地基的附加应力与桩身应力的分布特征；讨论了桩土应力此与桩土模量比，以及荷载及置换率的相互关系；揭了桩体变形和复合地基塑性区扩展的基本规律。即从不同角度探讨了复合地基的承力性状。     

Laboratory model tests for cyclic load-induced settlement of a strip foundation on a clayey soil

Laboratory model test results are presented for the cyclic load-induced settlement of a strip foundation supported by a saturated clayey soil. In performing the tests, the foundation was initially subjected to an allowable static load, after which a cyclic load with a frequency of one cycle per second was superimposed on it. The magnitudes of the static load and the amplitude of the cyclic load were varied. Based on the model test results, relationships for the foundation settlement and intensities of the static and cyclic loads are presented.     

Precipitation of Fe and Al compounds from the acid mine waters in the dogyae area, Korea: A qualitative measure of equilibrium modeling applicability and neutralization capacity?

To investigate the applicability of equilibrium modeling for the estimation of the chemical changes of acid mine waters, the phases predicted to precipitate by equilibrium calculation were compared with what actually precipitates from the stream and acid mine waters in the Dogyae area, Korea. The computer program MINTEQA2 was used for the equilibrium calculations based on the chemical compositional data of the water samples collected in the study area. XRD, IR, thermal and chemical analyses of the collected precipitates were performed to identify their phases.The results of the identification of the collected precipitates are inconsistent with what the equilibrium calculations predict. The equilibrium calculations indicate that ferrihydrite, FeOHSO₄, gibbsite, and AlOHSO₄ should precipitate from the stream and acid mine waters in the study area. However, the experimental analyses show that only ferrihydrite and Al₄(OH)₁₀SO₄ are the recognizable precipitates on the bottom of the stream and mine drainage channels. Comparing the stability relations among the possible precipitates with the field occurrence of the precipitates in the study area suggests that FeOHSO₄ and AIOHSO₄ are kinetically inhibited to precipitate and metastable ferrihydrite and Al₄(OH)₁₀SO₄ appear in their stability field instead. It indicates that the chemical compositional change of the waters due to the solid phase precipitation in the study area must be interpreted and predicted in terms of the precipitation of not the phases predicted by the equilibrium calculation but the actually identified ones.Assuming that the dissolved species in the aqueous phase are in equilibrium with respect to the currently precipitating solid phases in the study area, the water chemistries are attempted to interpret based on the plot of the theoretically calculated activities of the dissolved species on the stability diagram for the identified precipitates and gibbsite. The plot reveals a few evolution paths of the chemical composition of the acid mine water as the acid generation and neutralization progress. The evolution path producing ferrihydrite and then Al₄(OH)₁₀SO₄ precipitation suggests that the system including acid producing pyrite has lost significant amounts of its neutralizing capacity and thus, become intolerable to the impacts from acid mine water.