侧流化学磷回收强化生物除磷的模拟预测与试验验证

为了强化污水中生物除磷作用,本研究通过模拟预测与实验室试验验证了厌氧上清液侧流化学磷沉淀与回收对强化生物除磷的促进作用.模拟预测与试验结果表明,在进水COD/P=37.5工况下,当侧流比增加至30%时,通过化学磷沉淀（调节pH＞9.0）可使出水中TP浓度从碳源抑制时的＜6.0 mg·L-1（以P计）下降至≤1.0 mg·L-1（以P计）,同时可回收进水中P负荷的64%.经验证与校正后的TUD数学模型模拟预测有着与试验结果近乎一致的效果.因此,数学模拟技术完全有可能取代中间试验过程而直接将小试结果放大至工程应用.     

浸渍液pH值对V-Mo/Ti脱硝催化剂性能的影响研究

为提升V-Mo/Ti催化剂的脱硝性能,在催化剂制备过程中调节浸渍工艺参数,制备了一系列不同浸渍液pH值的催化剂,采用XRD、N2-吸附脱附、拉曼光谱、UV-Vis、H2-TPR、NH3-TPD等手段对催化剂进行表征,考察了pH值的变化对催化剂物理化学性能的影响,采用固定床微型反应器对催化剂的脱硝性能进行评价。结果表明,降低浸渍液pH值,可以抑制催化剂上VOx物种的聚合,提升催化剂的还原性能,有利于提升催化剂的脱硝效率,降低脱硝反应过程中N2O生成量。同时,浸渍液pH值的变化,也会影响催化剂的酸性性能。当浸渍液pH值低于3.64时,催化剂酸性性能显著降低,造成催化剂脱硝性能降低;当浸渍液pH值控制在3.64时,催化剂的还原性能和酸性性能匹配较好,从而显示了较高的脱硝性能。     

多源数据支持下城市火灾风险评估及规划响应

为探析城市火灾风险的空间格局特征,提出科学的火灾防控体系,以合肥市为研究对象,基于火灾风险兴趣点(POI)数据、NPP/VIIRS夜间灯光影像数据、消防站与道路信息等多源数据,运用SAVEE模型和迭代方程评估城市火灾风险,并引入区位-配置(L-A)模型,从不同目标情境优化消防站点布局。研究表明:火灾高风险区主要集中于合肥市二环以内的建成区,尤其是老城区、合肥西站片区、政务区、科学城和东部新中心等区域;现有48座消防站对研究区内的POI覆盖效果较好,覆盖率为86.76%,而对NPP/VIIRS覆盖效果一般,覆盖率仅为55.94%,覆盖率在合肥市东北部、西北部和南部部分地区仍有不足;基于最大化覆盖模型,规划新增44座消防站,明显提升5 min响应时间的覆盖率,可进一步夯实城市消防安全。     

An experimental study on the influence of zeolite on changes of pH and alkalinity in anaerobic treatment of compost leachate

With the increase of urbanization, municipal solid waste has also increased. Therefore, the need for solid waste management is also increasing compared with earlier decades. Composting is a good option for the recycling of solid waste; however, it produces leachate, which requires proper treatment systems to prevent environmental degradation. Due to high chemical oxygen demand (COD) concentrations in compost leachate, anaerobic treatment is the best option for handling the effluent, and an anaerobic baffled reactor (ABR) is one such anaerobic reactor that can be used for its treatment. Because of high ammonia and heavy metal concentrations, as well as the possibility of sludge washout in ABRs, it is important to use proper media, such as zeolite, which can reduce inhibition effects and sludge washout from the reactor. Anaerobic treatment, especially during the methanogenesis phase, is sensitive, and pH and alkalinity are parameters that influence the treatment. Therefore, adjusting these parameters within a normal range is very important to the proper functioning of anaerobic systems. In this study, a pilot‐scale ABR was used, and the last 4 of the 8 ABR compartments were filled with zeolite. The bioreactor was operated at hydraulic retention times (HRT) of 3, 4, and 5 days, with zeolite filling ratios of 10%, 20%, and 30%, and influent COD concentrations of 10,000, 20,000, and 30,000 milligrams per liter (mg/L). In this study, pH value was 6.43 ± 0.1, 6.96 ± 0.3, and 6.96 ± 0.25 at filling ratios of 10%, 20%, and 30%, respectively. According to the results, in all filling ratios, no significant changes were observed in the pH value when the organic loading rate increased and its amount was within a constant range. Influent alkalinity was equal to 2015 ± 510, 2884 ± 505, and 4154 ± 233 milligrams of calcium carbonate per liter (mg CaCO₃/L) at influent COD concentrations of 10,000, 20,000, and 30,000 mg/L, respectively, and in effluent, they were 2536 ± 336, 3379 ± 639, and 4377 ± 325 mg CaCO₃/L, respectively. The amount of alkalinity in the effluent increased compared with the alkalinity in the influent. The results show that the amount of alkalinity in the influent and effluent was similar, and the alkalinity enhancement was lower when the filling ratio was increased from 10% to 20%, and 20% to 30%. Comparisons of the results from zeolite with and without biofilm showed that, in cases of zeolite with biofilm, the amounts of silica and oxygen decreased and the amount of carbon increased, and it showed the formation of biofilm on the surface of zeolite. In addition, the absence of sodium in the zeolite with the biofilm indicated that sodium was exchanged with ammonium ions. According to the results, zeolite can be used in anaerobic reactors as a medium, and it also reduces fluctuations in pH and alkalinity at different organic loading rates, providing a normal range for anaerobic treatment.     

The Effects of Irrigation and Climate on the High Plains Aquifer: A County‐Level Econometric Analysis

The High Plains Aquifer (HPA) underlies parts of eight states and 208 counties in the central area of the United States (U.S.). This region produces more than 9% of U.S. crops sales and relies on the aquifer for irrigation. However, these withdrawals have diminished the stock of water in the aquifer. In this paper, we investigate the aggregate county‐level effect on the HPA of groundwater withdrawal for irrigation, of climate variables, and of energy price changes. We merge economic theory and hydrological characteristics to jointly estimate equations describing irrigation behavior and a generalized water balance equation for the HPA. Our simple water balance model predicts, at average values for irrigation and precipitation, an HPA‐wide average decrease in the groundwater table of 0.47 feet per year, compared to 0.48 feet per year observed on average across the HPA during this 1985–2005 period. The observed distribution and predicted change across counties is in the (?3.22, 1.59) and (?2.24, 0.60) feet per year range, respectively. The estimated impact of irrigation is to decrease the water table by an average of 1.24 feet per year, whereas rainfall recharges the level by an average of 0.76 feet per year. Relative to the past several decades, if groundwater use is unconstrained, groundwater depletion would increase 50% in a scenario where precipitation falls by 25% and the number of degree days above 36°C doubles. Editor’s note : This paper is part of the featured series on Optimizing Ogallala Aquifer Water Use to Sustain Food Systems. See the February 2019 issue for the introduction and background to the series.     

Changes in Hydrology of the Ganges Delta of Bangladesh and Corresponding Impacts on Water Resources

The Ganges Delta in Bangladesh is an example of water‐related catastrophes in a major rural river basin where limitations in quantity, quality, and timing of available water are producing disastrous conditions. Water availability limitations are modifying the hydrologic characteristics especially when water allocation is controlled from the upstream Farakka Barrage. This study presents the changes and consequences in the hydrologic regime due to climate‐ and human‐induced stresses. Flow duration curves (FDCs), rainfall elasticity, and temperature sensitivity were used to assess the pre‐ and post‐barrage water flow patterns. Hydrologic and climate indices were computed to provide insight on hydro‐climatic variability and trend. Significant increases in temperature, evapotranspiration, hot days, heating, and cooling degree days indicate the region is heading toward a warmer climate. Moreover, increase in high‐intensity rainfall of short duration is making the region prone to extreme floods. FDCs depict a large reduction in river flows between pre‐ and post‐barrage periods, resulting in lower water storage capacity. The reduction in freshwater flow increased the extent and intensity of salinity intrusion. This freshwater scarcity is reducing livelihood options considerably and indirectly forcing population migration from the delta region. Understanding the causes and directions of hydrologic changes is essential to formulate improve water resources management in the region.     

Climate and Land Use Effects on Hydrologic Processes in a Primarily Rain‐Fed,Agricultural Watershed

Anticipating changes in hydrologic variables is essential for making socioeconomic water resource decisions. This study aims to assess the potential impact of land use and climate change on the hydrologic processes of a primarily rain‐fed, agriculturally based watershed in Missouri. A detailed evaluation was performed using the Soil and Water Assessment Tool for the near future (2020–2039) and mid‐century (2040–2059). Land use scenarios were mapped using the Conversion of Land Use and its Effects model. Ensemble results, based on 19 climate models, indicated a temperature increase of about 1.0°C in near future and 2.0°C in mid‐century. Combined climate and land use change scenarios showed distinct annual and seasonal hydrologic variations. Annual precipitation was projected to increase from 6% to 7%, which resulted in 14% more spring days with soil water content equal to or exceeding field capacity in mid‐century. However, summer precipitation was projected to decrease, a critical factor for crop growth. Higher temperatures led to increased potential evapotranspiration during the growing season. Combined with changes in precipitation patterns, this resulted in an increased need for irrigation by 38 mm representing a 10% increase in total irrigation water use. Analysis from multiple land use scenarios indicated converting agriculture to forest land can potentially mitigate the effects of climate change on streamflow, thus ensuring future water availability.     

毛竹遗态 Fe2O3／Fe3O4／C 复合材料对水中锑（III）的吸附研究

以毛竹遗态Fe2 O3／Fe3 O4／C复合材料为吸附剂,锑（III ）初始含量、溶液初始pH值、吸附剂投加量以及吸附剂粒径为影响因素开展吸附影响研究。结果表明,随着锑（III ）初始浓度的升高,毛竹遗态Fe2 O3／Fe3 O4／C复合材料对锑（III ）的吸附量逐渐增加;初始溶液pH为7时,对锑（III ）的吸附效果最好,吸附量为4．7821 mg／g;块状吸附剂对水中锑（III ）的去除率和吸附量与粉末状吸附剂吸附效果相当。     

A~2/O联合臭氧污泥减量技术的改造研究

研究了臭氧化污泥减量技术联合A~2/O、倒置A~2/O与传统A~2/O在出水和污泥产率上的变化。结果表明,臭氧化A~2/O、臭氧化倒置A~2/O的出水与传统A~2/O相比未出现恶化,它们对COD和含氮物质的去除率分别为87.4%,53.7%和93%,66.5%,存在倒置A~2/O对臭氧混合液中有机质及含氮物质的利用率较A~2/O高的可能。试验按每克SS投加0.05 g O_3对A2/O与倒置A~2/O产生的约60%剩余污泥处理时,在短期内未造成出水磷含量的大幅升高,并且出水磷含量受臭氧混合液DO、二沉池底部DO的影响,两系统的污泥产率分别较传统A~2/O降低50%,56%。     

Bi/Fe_3O_4催化NaBH_4还原水中对硝基苯酚

以磁性Fe_3O_4为载体负载Bi(NO_3)_3,再用NaBH_4还原Bi~(3+)制备了Bi/Fe_3O_4催化剂。采用XRD和紫外-可见光谱对催化剂进行表征。考察了Bi负载量、NaBH_4加入量和Bi/Fe_3O_4加入量对Bi/Fe_3O_4催化NaBH_4还原对硝基苯酚(4-NP)效果的影响。表征结果显示:当催化剂中Bi含量较少时,Bi分散良好;当Bi含量较多时,会形成纳米颗粒。实验结果表明:当反应温度为25℃,初始4-NP浓度为4.0 mmol/L时,在Bi负载量为5%(w)、Bi/Fe_3O_4催化剂加入量为500 mg/L,NaBH_4加入量为6.0 g/L的条件下,反应速率常数为0.581 min~(-1),4-NP的去除率为99.7%;Bi/Fe_3O_4催化剂稳定性好,重复使用15次后,活性基本不变。