雅砻江锦屏二级水电站减水河段生态需水量研究

针对雅砻江锦屏二级水电站减水河段面临的水生生物生态需水问题,提出了计算河道最小生态基流量的生态水力学法,考虑了水力生境参数的全河段变化情况,计算结果避免了单凭最低值进行判断所造成的判断失误。确定了锦屏二级水电站减水河段鱼类对流速、水深、水面宽等水力生境的需求。通过河道水力模拟,得出为满足减水河段鱼类的生存及繁衍,必须保证枯水季节猫猫滩闸址下泄45 m3/s流量,在该流量下,锦屏二级水电站减水河段中95%左右河段水力因子可满足研究中提出的河道内鱼类的生存条件;水温的变化不会影响河道内鱼类产卵;鱼类适应的缓流水、急流水、浅滩、深潭等水力形态的位置虽然发生变化,但数量保持不变。     

pH-dependent leaching behaviour and other performance properties of cement-treated mixed contaminated soil

Portland cement has been widely used for stabilisation/solidification (S/S) treatment of contaminated soils. However, there is a dearth of literature on pH-dependent leaching of contaminants from cement-treated soils. This study investigates the leachability of Cu, Pb, Ni, Zn and total petroleum hydrocarbons (TPH) from a mixed contaminated soil. A sandy soil was spiked with 3000 mg/kg each of Cd, Cu, Pb, Ni and Zn, and 10,000 mg/kg of diesel, and treated with ordinary Portland cement (CEM I). Four different binder dosages, 5%, 10%, 15% and 20% (m/m) and different water contents ranging from 13%-19% dry weight were used in order to find a safe operating envelope for the treatment process. The pH-dependent leaching behaviour of the treated soil was monitored over an 84-day period using a 3-point acid neutralisation capacity (ANC) test. The monolithic leaching test was also conducted. Geotechnical properties such as unconfined compressive strength (UCS), hydraulic conductivity and porosity were assessed over time. The treated soils recorded lower leachate concentrations of Ni and Zn compared to the untreated soil at the same pH depending on binder dosage. The binder had problems with Pb stabilisation and TPH leachability was independent of pH and binder dosage. The hydraulic conductivity of the mixes was generally of the order, 10^-8 m/sec, while the porosity ranged from 26%-44%. The results of selected performance properties are compared with regulatory limits and the range of operating variables that lead to acceptable performance described.     

BAF去除氨氮关键影响因素研究

为探讨曝气生物滤池去除氨氮的关键因素,选取沈阳仙女河污水处理厂(40万t/d)现场进行实地研究。通过测定不同条件下(pH、进水COD浓度、溶解氧、温度、水力负荷)的氨氮去除率,并进行主成分分析结果显示,影响BAF工艺脱氮的关键因素是温度、溶解氧和水力负荷。当温度在14~30℃之间时,氨氮的去除率一直维持较高,当温度低于14℃时,氨氮的去除率较低;随着溶解氧浓度的增大,氨氮的去除率也随之升高,当溶解氧增加到5.6 mg/L时,氨氮的去除率达到80%~90%,接近饱和状态;在水力负荷为3.08~4.15 m3/(m.2h)之间时,氨氮的去除率上升,超过该值,则氨氮去除率下降。     

水力停留时间和溶解氧对陶粒CANON反应器的影响

以人工配制无机高氨氮废水为进水,通过接种CANON污泥,以陶粒作为填料,研究了HRT和DO对生物膜CANON反应器的影响.试验过程中,控制进水氨氮浓度基本不变,依次控制反应器的HRT为9、7、5 h,同时控制DO的范围为1.16~3.20 mg·L-1.研究发现:1当DO为1.20~1.75 mg·L-1时,尽管提高DO有利于提高AOB的活性和系统内基质的传质效果,但是CANON反应器的NH+4-N、TN去除效果依然随着HRT的缩短而下降,尤其当DO超过2.50 mg·L-1时,TN去除效果大幅度下降;2当DO为1.20~1.75 mg·L-1时,随着HRT的缩短,CANON反应器的短程硝化性能趋于稳定,而当DO超过1.75 mg·L-1时,即使缩短HRT,其短程硝化性能依然遭到严重破坏;3CANON反应器中短程硝化稳定性能和去除效果较佳的条件是HRT为7 h,且DO控制在1.20~1.75 mg·L-1之间.HRT和DO是废水生物处理的重要运行参数,直接影响到生物处理的效果和出水水质,协调控制两者的变化范围,对提高CANON工艺对高氨氮废水的处理效果非常重要.     

ANAMMOX富集与优化停曝比对MBR-SNAD工艺的影响

采用膜生物反应器（MBR）研究了厌氧氨氧化细菌在富集过程中的活性变化,在启动全程自养脱氮（CANON）工艺中以恒定曝气量,通过优化停曝比实现氨氧化细菌（AerAOB）和厌氧氨氧化细菌（AnAOB）协同脱氮并且有效抑制亚硝酸盐氧化菌（NOB）的活性,然后添加有机物（乙酸钠）逐步启动同步亚硝化-厌氧氨氧化耦合异养反硝化（SNAD）工艺.结果表明,在厌氧氨氧化细菌富集过程中,通过不断缩短水力停留时间（HRT）提高进水氮负荷的方式强化厌氧氨氧化细菌活性,其平均活性由0.603mgN/（h·gVSS）提高到了8.1mgN/（h·gVSS）;当恒定曝气量为50mL/min,停曝比为4：10（min：min）时,AerAOB和AnAOB对氨氮的去除量分别占总氨氮去除量的58.8%和41.2%,NOB氧化亚硝态氮的量占总硝态氮生成量的15.3%,成功抑制了NOB的活性;当C/N比为0.5,调整停曝比为4：15后,反硝化过程氮去除量占总氮去除率的20.9%,厌氧氨氧化过程氮去除量占总氮去除率的79.1%,实现了AerAOB、AnAOB和反硝化细菌（DNB）协同脱氮的目的.     

蓄水、调水、发电，扼制生态环境恶化

蓄水是根本，调水是手段，发电是关键。植树造林和拦河筑坝建设水库电站以及沟渠塘蓄水，可以防止水土流失和水能浪费；调水可以解决横向和纵向水资源分布不平衡带来的问题；发电可以解决调水所需动力和全国缺电的问题。其经济效益约合２０００亿元，而且还能扼制生态环境的恶化，减少每年４６．６×１０４ｈｍ２土地的损失，缓解荆江大堤和黄河下游大堤越筑越高之危。     

Modelling the migration of contaminants through variably saturated dual-porosity, dual-permeability chalk

In the Hesbaye region in Belgium, tracer tests performed in variably saturated fissured chalk rocks presented very contrasting results in terms of transit times, according to artificially controlled water recharge conditions prevailing during the experiments. Under intense recharge conditions, tracers migrated across the partially or fully saturated fissure network, at high velocity in accordance with the high hydraulic conductivity and low effective porosity (fracture porosity). At the same time, a portion of the tracer was temporarily retarded in the almost immobile water located in the matrix. Under natural infiltration conditions, the fissure network remained inactive. Tracers migrated downward through the matrix, at low velocity in relation with the low hydraulic conductivity and the large porosity of the matrix. Based on these observations, Brouyère et al. (2004a) [Brouyère, S., Dassargues, A., Hallet, V., 2004a. Migration of contaminants through the unsaturated zone overlying the Hesbaye chalky aquifer in Belgium: a field investigation, J. Contam. Hydrol., 72 (1-4), 135-164, doi: 10.1016/j.conhyd.2003.10.009] proposed a conceptual model in order to explain the migration of solutes in variably saturated, dual-porosity, dual-permeability chalk. Here, mathematical and numerical modelling of tracer and contaminant migration in variably saturated fissured chalk is presented, considering the aforementioned conceptual model. A new mathematical formulation is proposed to represent the unsaturated properties of the fissured chalk in a more dynamic and appropriate way. At the same time, the rock water content is partitioned between mobile and immobile water phases, as a function of the water saturation of the chalk rock. The groundwater flow and contaminant transport in the variably saturated chalk is solved using the control volume finite element method. Modelling the field tracer experiments performed in the variably saturated chalk shows the adequacy and usefulness of the new conceptual, mathematical and numerical model.     

液压支架薄煤层采煤工作面风流流动规律研究

分别对北宿煤矿以装备液压支架和单体支柱为主的14710和1667薄煤层采煤工作面风流场进行了现场测定研究,结果显示,装备液压支架后,工作面的风流流动规律发生了较大变化,百米风阻值及向采空区的漏风率均大幅度提高。     

Field Studies on 32P Movement and P Leaching from Flooded Paddy Soils in the Region of Taihu Lake, China

Field experiments were done in two sites, Yixing and Changshu, Jiangsu province, China, to study P movement and leaching in flooded paddy soils. P movement in soil was investigated by using the KH₂ ³²PO₄ tracker method, and the amount of P leached from the soil layer in different depths was estimated by measuring P concentrations in the soil solution and saturated hydraulic conductivities in field. Determination was done about one month after P application. There was 46% and 42% of total ³²P retained in the 0–5cm layer of soil in the Yixing site and in the Changshu site respectively. The ³²P retained in the 25–30 cm layer was only about 1–2% of the total ³²P added. Furthermore, 8.01% of ³²P in the soil of Yixing site and 16.8% of ³²P in the soil of Changshu site was lost from the layer 0–30cm soil. The seasonal amounts of P leached from the top soil layer and from bottom layer are about 4.5–5.8% and 1.6–2.1% of the total P application, respectively. Changes of total P concentrations in soil solutions during rice growth showed that the fertilizer P applied before flooding of the paddy fields suffered a flash leaching loss and a slow leaching loss. We concluded that the fertilizer P could quickly move in the flooded paddy rice field and parts of it can enter into surface water and ground water. Unless the P application is well managed the risk of P loss and consequently environmental pollution exist.     

冬季菹草对悬浮泥沙的影响

利用冬季沉水植物菹草构建由浅水到深水的串联系统,含沙水依次流经浅水区和深水区,测定各级菹草对水体悬浮泥沙含量和沉降量的影响.结果显示,菹草系统可以降低水体中悬浮泥沙含量,并随水力停留时间延长而降低程度加大.各运行条件下,菹草系统悬浮泥沙平均沉降量65.7 g·m-2,比对照组高39.4%.菹草表面泥沙的吸附是一个"吸附-沉降-再吸附" 的动态过程,吸附量为3.26～5.69 g·kg-1.菹草对冬季水生态系统的自净功能起着十分重要的作用.