磷矿矿山顶板稳定性分级方法

冒顶片帮事故是地下矿山危害最为严重的事故,矿山地压管理是地下开采矿山安全管理的重要任务.顶板稳定性分析是地压管理的重要方法.提出了顶板稳定性分级的指标和分级方法.首次指出风化作用对顶板稳定性的影响,并就地下水对顶板稳定性的影响进行了分析.     

Quantifying Reductions of Mass‐Failure Frequency and Sediment Loadings From Streambanks Using Toe Protection and Other Means: Lake Tahoe,United States1

Abstract: Streambank erosion by mass‐failure processes represents an important form of channel adjustment and a significant source of sediment in disturbed streams. Mass failures regularly occur by a combination of hydraulic processes that undercut bank toes and geotechnical processes that cause bank collapse by gravity. Little if any quantitative information is available on the effectiveness of bank treatments on reducing erosion. To evaluate potential reduction in sediment loadings emanating from streambanks, the hydraulic and geotechnical processes responsible for mass failure were simulated under existing and mitigated conditions using a Bank‐Stability and Toe‐Erosion Model (BSTEM). Two critical erosion sites were selected from each of the three watersheds known to contribute the greatest amounts of fine sediment by streambank processes in the Lake Tahoe Basin. A typical high‐flow annual hydrograph was selected for analysis. Bank‐material strength data were collected for each layer as were species‐specific root‐reinforcement values. The effects of the first flow event on bank‐toe erosion were simulated using an excess shear‐stress approach. The resulting geometry was then exported into the bank‐stability submodel to test for the relative stability of the bank under peak flow and drawdown conditions. In this way, BSTEM was used iteratively for all flow events for both existing and mitigated conditions. On average, 13.6% of the material was eroded by hydraulic shear, the remainder by mass failures, which occurred about five times over the simulation period. Simulations with 1.0 m‐high rock‐toe protection showed a dramatic reduction in streambank erosion (69‐100%). Failure frequency for the simulation period was reduced in most cases to a single episode. Thus, an almost 90% reduction in streambank loadings was achieved by virtually eliminating the erosion of only 14% of the material that was entrained by hydraulic forces. Consequently, simulations show average load reductions of about an order of magnitude. Results stress the critical importance of protecting the bank toe‐region from steepening by hydraulic forces that would otherwise entrain previously failed and in situ bank materials, thereby allowing the upper bank to flatten (by failure) to a stable slope.     

Bed Stability and Sedimentation Associated With Human Disturbances in Pacific Northwest Streams1

Abstract: To evaluate anthropogenic sedimentation in United States (U.S.) Pacific Northwest coastal streams, we applied an index of relative bed stability (LRBS*) to summer low flow survey data collected using the U.S. Environmental Protection Agency’s Environmental Monitoring and Assessment Program field methods in a probability sample of 101 wadeable stream reaches. LRBS* is the log of the ratio of bed surface geometric mean particle diameter (D_gm) to critical diameter (D*_cbf) at bankfull flow, based on a modified Shield’s criterion for incipient motion. We used a formulation of LRBS* that explicitly accounts for reductions in bed shear stress that result from channel form roughness due to pools and wood. LRBS* ranged from ?1.9 to +0.5 in streams within the lower quartile of human riparian and basin disturbance, and was substantially lower (?4.2 to ?1.1) in streams within the upper quartile of human disturbance. Modeling results suggest that the expected range of LRBS* in streams without human disturbances in this region might be generally between ?0.7 and +0.5 in either sedimentary or volcanic lithology. However, streams draining relatively soft, erodible sedimentary lithology showed greater reductions in LRBS* associated with disturbance than did those having harder, more resistant volcanic (basalt) lithology with similar levels of basin and riparian disturbance. At any given level of disturbance, smaller streams had lower LRBS* than those with larger drainages. In sedimentary lithology (sandstone and siltstone), high‐gradient streams had higher LRBS* than did low‐gradient streams of the same size and level of human disturbance. High gradient streams in volcanic lithology, in contrast, had lower LRBS* than low‐gradient streams of similar size and disturbance. Correlations between D_gm and land disturbance were stronger than those observed between D*_cbf and land disturbance. This pattern suggests that land use has augmented sediment supplies and increased streambed fine sediments in the most disturbed streams. However, we also show evidence that some of the apparent reductions in LRBS*, particularly in steep streams draining small volcanic drainages, may have resulted in part from anthropogenic increases in bed shear stress. The synoptic survey methods and designs we use appear adequate to evaluate regional patterns in bed stability and sedimentation and their general relationship to human disturbances. More precise field measurements of channel slope, cross‐section geometry, and bed surface particle size would be required to use LRBS* in applications requiring a higher degree of accuracy and precision, such as site‐specific assessments at individual streams.     

聚硅基复合氯化铁絮凝剂的制备及其在采油废水处理中的应用

采用硅酸钠制备聚硅酸,探讨了活化pH、活化剂、硅酸钠浓度(以SiO_2质量分数计)及聚合温度等因素对聚硅酸稳定性的影响.利用聚硅酸及氯化铁制备聚硅基复合氯化铁(PSiF),并通过正交试验分析了活化pH、Si/Fe(摩尔比)、OH/Fe(摩尔比)、制备时间对PSiF絮凝性能的影响.综合考虑絮凝性能、稳定性以及经济性等因素,确定PSiF适宜的制备条件为SiO_2质量分数2%～3%;活化pH为2～3;Si/Fe为0.50～0.75;OH/Fe为0.50～0.75;制备时间为0.5 h;聚合温度低于25℃.对比PSiF、PAC、FeCl_3对采油废水的处理效果,PSiF除浊、除COD效果以及经济性最好,是一种应用前景广阔的新型絮凝剂.     

多层采空区条件下的高速公路路堑边坡稳定性数值分析

高速公路建设过程中常穿越各种矿山采空区,采空区对路堑边坡的稳定性产生较大的影响。基于有限差分分析的快速拉格朗算法FLAC3D程序,由于具有强大的数值模拟分析功能,可以模拟多种结构形式的地质体,因而广泛应用于各种岩土工程问题。本文结合国家某重点交通项目,采用快速拉格朗算法FLAC3D程序对多层采空区条件下的某路堑边坡稳定性进行了评价,主要包括开挖、注浆和锚固等工况下路堑边坡的应力和位移分析。分析结果表明,采空区经过处理后的路堑边坡是稳定的,FLAC3D应用于多层采空区条件下的路堑边坡稳定性评价是可行的。     

滤料粒径对给水曝气生物滤池运行稳定性的影响

利用给水曝气生物滤池(UBAF)处理刘屋洲水源水,考察了不同陶粒粒径对氨氮、高锰酸盐指数的去除效果以及水头损失变化的影响。结果表明,陶粒3～5 mm的UBAF对氨氮、高锰酸盐指数的去除效果较高,但是其水头损失较大,且反冲洗前后水头损失变化偏大,不利于UBAF稳定运行。陶粒6～10 mm的UBAF运行状况良好,氨氮的去除率为73.8%,高锰酸盐指数的去除率为18.6%,滤池24 h过滤水头损失<0.4 m,反冲洗前后过滤水头损失变化量<5 cm。其出水氨氮和高锰酸盐指数均达到《生活饮用水卫生标准》(GB5749-2006),滤池的水头损失小,反冲洗前后也变化甚微。进一步的实验表明陶粒破碎会导致滤料粒径级配变化,使得水头损失增加。     

石油污染土壤胶体特征及其稳定性

采集辽河油田石油污染土壤样品并用离心法提取胶体,定性和定量研究了石油污染土壤胶体的主要物理化学性质,通过间歇实验研究了不同p H(p H=4~9)、不同价态阳离子(Na+、Ca2+和Fe3+)和不同价态阴离子(NO-3、SO2-4和PO3-4)存在下的胶体稳定性,比较了阳离子存在下石油污染土壤胶体和未受污染土壤胶体稳定性。研究结果表明,该石油污染土壤胶体总石油烃含量为123.24 mg/g,石油烃主要为直链烷烃和环烷烃。相同p H条件下石油污染土壤胶体Zeta电位负值比未受污染土壤胶体Zeta电位负值高。石油污染土壤胶体稳定性随p H值增加而增加,随着阳离子价数升高而减小,随阴离子价数升高而增大。Ca2+和Cu2+存在下,石油污染土壤胶体比未受污染土壤胶体稳定性更小。Na+和Fe3+存在下,石油污染土壤胶体比未受污染土壤胶体稳定性更大。     

贡湖湾退渔还湖区的基底稳定性的时空特征

2012年11月至2014年5月期间季度性对无锡贡湖湾退渔还湖生态修复工程进行跟踪调查与检测,就贡湖湾湿地土壤环境退渔还湖修复工程前后的理化性质进行了分析比较,用以评估修复工程实施后退渔还湖区基底的改善效果.结果表明:退渔还湖区内基底化学性质,有机质、总氮、总磷比退渔还湖初期分别提高241.59％、98.61％和162.86％.其中,有效氮和有效磷的均值为102.31 mg/kg和15.10 mg/kg,满足土壤养分分级标准Ⅲ级标准.有关基底稳定性物理性质与退渔还湖初期相比,土壤容重减少17.84％,pH值稳定在5.8 ～6.5之间,土壤缓冲能力明显提高,修复区南部(人为种植植物)的土壤团聚体稳定性恢复状况最好,西部(自然恢复)次之,北部(基底状况差,无植物种植)恢复状况低于前述两区.总之,贡湖退渔还湖修复区在经过17个月后,其基底的整体质量趋于良好,土壤各项养分及团聚体稳定性指标逐步达到合理水平,土壤环境已具有良好的生态功能.     

中试螺旋式自循环厌氧反应器处理安乃近制药废水的稳定性能简

以制药废水实验了50 m³螺旋式厌氧反应器（SPAC反应器）的稳定性。采用Augmented Dickey-Fuller（ADF）单位根检验表明,螺旋式反应器具有良好的启动和运行稳定性。负荷冲击实验显示,SPAC反应器具有较好的耐浓度冲击能力和耐水力冲击能力,所能耐受的最大浓度冲击强度大于60 000 （mg·h）/L（进水浓度提升2倍）,所能耐受的最大水力冲击强度为300（m³·h）/d（进水流量提升50%）。SPAC反应器还具备受扰恢复能力。在反应液pH低于5.74,出水浓度、COD去除率和容积COD去除速率（VRR）分别为3 500 mg/L、22.30%和2.52 kg/（m³·d）的工况下,经过30 d恢复,出水浓度、COD去除率和VRR的恢复程度达到80%~90%。     

Long-term Hg pollution induced Hg tolerance in the terrestrial isopod Porcellio scaber (Isopoda, Crustacea)

The aim of our work was to assess the pollution-induced community tolerance (PICT) of isopod gut microbiota and pollution-induced isopod population tolerance (PIPT). Animals collected from a chronically Hg polluted and an unpolluted location were exposed for 14 days to 10microg Hg/g dry food under laboratory conditions. The lysosomal membrane stability, hepatopancreas epithelium thickness, feeding activity and animal bacterial gut microbiota composition were determined. The results confirm the hypothesis that the response to short-term Hg exposure differs for animals from the Hg polluted and the unpolluted field locations. The animals and their gut microbiota from the Hg polluted location were less affected by Hg in a short-term feeding experiment than those from the unpolluted environment. We discuss the pollution-induced population tolerance of isopods and their gut microbiota as a measure of effects of long-term environmental pollution. The ecological consequences of such phenomena are also discussed.