改革开放以来广州市番禺区景观格局变化研究

番禺区作为广州市新的发展方向,处于中国经济和社会发展的前沿。研究番禺区20年来的景观格局变化,对于其经济社会的可持续、健康发展有一定的指导意义。利用番禺区1979年、1990年、2000年的MSS、TM、ETM^＋影像,在GIS的支持下,结合景观生态学的理论分析了番禺区三个时期的景观格局及其动态变化。结果表明,20年来,番禺区的景观格局变化迅速,斑块数量和空间格局变化较大;各景观类型之间的转移明显,耕地、林地快速向建设用地、养殖水域等转变。人文因素是景观格局变化的直接驱动力,人口增长、经济发展是导致景观系列变化最根本的原因。     

氨与脉冲电晕等离子体脱除SO_2的协同效应

为了揭示氨与等离子体脱除ＳＯ２的协同效应，对比了脉冲电晕等离子体在氨气注入前后ＳＯ２脱除率的变化。实验结果表明，脉冲电晕等离子体单独作用时，ＳＯ２脱除率仅为９％～１５％，而氨与脉冲电晕等离子体共同作用时，ＳＯ２脱除率可达９０％以上（ｆ＝１．０）．并从化学热力学角度探讨了氨与脉冲电晕的协同效应能显著提高ＳＯ２脱除率的原因，还考察了氧含量、温度对协同效应的影响     

Initial identification of heavy metals contamination in Taihu Lake, a eutrophic lake in China

A detailed investigation of seven heavy metals (Cu, Cd, Cr, As, Pb, Zn, Ni) in the water column, interstitial water and surface sediment was conducted to quantify the extent of their contamination in Taihu Lake. Results showed the average total concentrations ranged from 0.93 μg/L for Cd to 47.03 μg/L for Zn. The dissolved concentrations in the overlying water ranged from 0.06 μg/L for Cd to 15.86 μg/L for Zn. The metals in the Taihu Lake surface water were primarily in the particulate phase, especially for Cd, whose particulate concentration represented 94.3% of the total. In the surface sediment, the mean concentrations for Cr, Ni, Cu, Zn, As, Cd and Pb were 41.50, 28.72, 27.82, 65.46, 5.94, 0.82 and 41.17 mg/kg, respectively. The metals in the water column and sediments of Taihu Lake displayed significant spatial variations, and the higher metal concentrations mainly occurred in the north and west of Taihu Lake, especially in Zhushan Bay and West Taihu Lake. A quality assessment indicated that most of the metals in the surface water of Taihu Lake had no or low adverse health effects on organisms, except for Pb and Cu, which may cause chronic toxicity. Compared with the "Consensus-Based Sediment Quality Guidelines", the polluting metals were Cr, Ni and Cd, and the polluted regions were confined to Zhushan Bay, Meiliang Bay and the west of Taihu Lake, especially for north of Zhushan Bay. The polluted areas for Cr, Ni and Cd were 14.36, 34.70 and 13.24 km², respectively. We suggest that Cr, Ni, and Cd in the polluted areas should be addressed and that tissue chemistry and sediment toxicity assessments be performed as soon as possible.     

基于EFDC城市景观湖泊水动力模拟研究

城市景观湖泊是生态城市建设的重要组成部分,其水流缓慢,水动力交换和自净能力较弱,水质易受城市排污、径流、人为活动等因素影响。本文应用EFDC(environment fluid dynamic code)三维模型研究分析了典型城市景观湖泊-天印湖的水动力特征,模拟了2011年9月至2013年12月水龄变化过程和时空分布,分析降雨径流和风力驱动对水龄的影响力。结果表明:天印湖的水动力主要驱动力为降雨径流,风力对水龄的影响很小。研究结论有助于理解城市景观水体的水动力特性以及进一步研究水动力对水质变化的影响,并为城市水环境建设和保护提供一定的方案支持。     

滇池水环境污染成因及治理策略分析

滇池水污染严重制约了昆明市居民生活质量的提高和和经济的可持续发展,准确把握引起滇池水体污染的原因是制定治污方案的关键。近年来,由于滇池地区人口的增长和经济的迅速发展,排入滇池的污染物和致营养化物质不断增加,加之人们对森林的过度砍伐,极度破坏了滇池生态环境的平衡,降低了生态环境净化能力,致使滇池水体污染进一步加重。因此,治理滇池水体污染,首先要控制污染源以减少污染物和致营养化物质的排放,加大污染物和致营养化物质排放前的处理工作;其次加大森林保护力度,退耕还林;增强生态环境自身净化能力也是滇池水体污染治理的好方法。     

脉冲电晕放电去除NO的反应途径研究

对脉冲放电等离子体条件下去除NO的宏观反应机理进行研究结果表明,不同氧含量的氮气流中NO的脱除均同时存在氧化、分解与还原三条途径。气流中氧含量不同,起主导的反应也不相同。还考察了NH₃气、H₂O蒸气等调质剂对反应途径的影响。NH₃的加入有利于NO通过还原途径脱除,但同时导致生成N2O反应的加剧,而产生二次污染,由此说明NH3加入位置的重要性。水蒸气在等离子体作用下产生氧化性物种,有利于NO的氧化脱除。本实验条件下加入气流量1％的水气即能使NO氧化脱除率增加20％左右。实验还考察了电参数（峰值电压、脉冲重复频率等）对NO脱除反应的影响。最后对本实验条件下的反应机理进行推断,所得结果对脉冲电晕等离子体烟气脱NO工艺研究具有一定的指导意义。     

Feasibility of a membrane-aerated biofilm reactor to achieve single-stage autotrophic nitrogen removal based on Anammox

A laboratory-scale membrane-aerated biofilm bioreactor (MABR) equipped with non-woven fabrics support around the gas-permeable carbon tube was developed for single-stage autotrophic nitrogen removal based on partial nitrification and anaerobic ammonium oxidization. This reactor allowed air to be supplied through the microporous carbon tube wall to the biofilm that was supported by non-woven fabrics. The partial nitrification and consumption of dissolved oxygen occurred in the inner layer and Anammox in the anoxic outer layer of the non-woven fabrics, thus realizing autotrophic nitrogen removal in a single reactor. After 116d of operation, the maximal nitrogen removal of 0.77kgNm(-3)d(-1) at a volumetric ammonium loading rate of 0.87kgNm(-3)d(-1) was achieved. The spatial profiles of the ammonia-oxidizing bacteria and Anammox bacteria were evaluated by fluorescence in situ hybridization. This study demonstrated that MABR was a very suitable experimental set-up for the operation of the single-stage autotrophic nitrogen removal process.     

生物催化氧化法脱除H2S的试验研究

针对H₂S污染的严峻形势，构建了包括催化再生装置和生物滴滤器的生物催化氧化装置。该装置以沸石为填料，以氧化亚铁硫杆菌为脱硫菌种，通过微生物和Fe³⁺的双重氧化作用高效脱除H₂S。试验确定了装置的适宜喷淋量和沸石的最佳粒径。在温度为30℃，进气量为0.25 m³/h，进气H₂S浓度为2500mg/m³，喷淋量为1000mL/h，喷淋液的pH值为1.97、Fe³⁺浓度为0.05 mol/L的条件下，出气H₂S浓度足以达到GB14554-93规定的一级厂界标准值。试验证明，生物催化氧化法是一种新型高效的脱硫技术，应进一步开展中试研究。     

Response of non-point source pollutant loads to climate change in the Shitoukoumen reservoir catchment

The impacts of climate change on streamflow and non-point source pollutant loads in the Shitoukoumen reservoir catchment are predicted by combining a general circulation model (HadCM3) with the Soil and Water Assessment Tool (SWAT) hydrological model. A statistical downscaling model was used to generate future local scenarios of meteorological variables such as temperature and precipitation. Then, the downscaled meteorological variables were used as input to the SWAT hydrological model calibrated and validated with observations, and the corresponding changes of future streamflow and non-point source pollutant loads in Shitoukoumen reservoir catchment were simulated and analyzed. Results show that daily temperature increases in three future periods (2010–2039, 2040–2069, and 2070–2099) relative to a baseline of 1961–1990, and the rate of increase is 0.63°C per decade. Annual precipitation also shows an apparent increase of 11 mm per decade. The calibration and validation results showed that the SWAT model was able to simulate well the streamflow and non-point source pollutant loads, with a coefficient of determination of 0.7 and a Nash–Sutcliffe efficiency of about 0.7 for both the calibration and validation periods. The future climate change has a significant impact on streamflow and non-point source pollutant loads. The annual streamflow shows a fluctuating upward trend from 2010 to 2099, with an increase rate of 1.1 m³ s⁻¹ per decade, and a significant upward trend in summer, with an increase rate of 1.32 m³ s⁻¹ per decade. The increase in summer contributes the most to the increase of annual load compared with other seasons. The annual NH₄⁺-N load into Shitoukoumen reservoir shows a significant downward trend with a decrease rate of 40.6 t per decade. The annual TP load shows an insignificant increasing trend, and its change rate is 3.77 t per decade. The results of this analysis provide a scientific basis for effective support of decision makers and strategies of adaptation to climate change.     

Evaluating the effectiveness of routine water quality monitoring in Miyun reservoir based on geostatistical analysis

This study used geographic information system techniques and geostatistics methods to evaluate the effectiveness of routine water quality monitoring in the western segment of the Miyun reservoir in Beijing. Methodologies as well as the sampling design are evaluated. The single-layer evaluation and three integrated evaluation methods including principal component analysis (PCA), ordinary kriging (OK)_Mean, and Mean_Layers were used to validate the effectiveness of evaluation methods, and the effectiveness of each sampling design was validated by comparing their errors. Results indicated that, while a single-layer evaluation only shows the trophic state of water at a specific level, an integrated evaluation synthetically analyzes and evaluates the trophic state of the entire water body. Furthermore, results of the integrated analysis show that a PCA method is more accurate and can represent the trophic state of the entire water body. The OK_Mean and Mean_Layers methods are only able to represent the mean level for trophic state of the entire water body but cannot reflect local trophic state and distribution details. Although methods used in the routine monitoring of Miyun reservoir have some similarities to the OK_Mean and Mean_Layers methods, their range of errors and uncertainty are greater because of a lack of detailed spatial continuous information. The analysis on the number of sampling points shows that, within a certain range of error, minor changes of sampling points will have no obvious impact on the monitoring results. For the routine monitoring of western Miyun reservoir, using only three to five sampling points for monitoring is inadequate. According to our analysis, it is more appropriate to use at least ten sampling points for monitoring these areas.