考虑相位的屏障衍射声场工程算法研究

目前声屏障衰减的工程算法均基于能量法,不考虑声源在衍射时的相位变化,而在计算有限长屏障衍射声场或多个屏障的多重衍射声场时,往往误差较大。因此,提出了一种考虑相位、用于计算屏障声衍射的新工程计算方法,该工程算法基于Keller的几何声衍射理论,且延伸自Pierce提出的一个刚性楔形体边界的Hadden-Pierce严格解,相比严格解的积分算法,该简化算法能在计算声影边界的衍射声时避免奇异,计算效率高。使用本文提出的算法、边界元法和Wadsworth研究的实验数据对三维有限长薄屏障和单个厚屏障的双重衍射声场进行了计算,结果表明,该算法与Hadden-Pierce原始积分算法误差在0.5 dB范围以内,与边界元法误差在2 dB以内,且与Wadsworth实验数据吻合度较高;而在计算效率方面,本算法相比原始积分算法提高了500多倍,比边界元法提高了约2400倍,说明本简化算法完全可应用于户外噪声传播中屏障衰减的准确计算。     

介质阻挡放电联合锰基催化剂对乙酸乙酯的降解效果

采用等体积浸渍法制备锰基催化剂MnO_x/13X和MnO_x/γ-Al₂O₃,并在吸附-间歇放电模式下研究了其联合介质阻挡放电(DBD)等离子体对乙酸乙酯的氧化性能;对催化剂进行BET、SEM和XPS表征,以分析不同载体的Mn基催化剂氧化效果存在差异的原因。DBD氧化实验结果表明：与13X和γ-Al₂O₃相比,负载活性组分MnO_x后,CO_x产率分别提高了36.3%(MnO_x/13X)和29%(MnO_x/γ-Al₂O₃),CO₂选择性均提高至98%以上,副产物臭氧明显减少。表征结果显示,MnO_x/13X上的Mn⁴⁺和晶格氧含量更高,更有利于乙酸乙酯的降解。结合吸附态乙酸乙酯的等离子体降解机理和不同填充材料的实验数据,建立了相应的动力学模型,为DBD降解挥发性有机物系统中催化剂的优化及其应用提供参考。     

新型介质阻挡放电反应器同时处理废气和废液研究

为了充分发挥介质阻挡放电处理污染物的能力.本研究依据介质阻挡放电降解废气和废液的原理,设计了一种介质阻挡放电同时处理废液和废气的反应器,并对模拟废气甲苯和染料废水进行处理.实验过程中对甲苯和染料废水分别单独处理和两者同时处理的效果进行了比较.结果表明,甲苯在单独处理和同染料废水同时处理时都可达到较高的降解效果,两者同时处理时甲苯的降解效率可达88.6%.并且在甲苯降解效率基本保持不变的情况下,本反应器可以实现对染料废水的同步降解,其中处理50 mg·L-1活性艳蓝60min时,降解率可达95.4%,每小时处理量为35.8 mg.通过同时处理甲苯和染料废水提高了反应器的能量利用效率.     

泗河水环境容量及最大允许排污量计算

规范了水环境容量的定义和分类,建立了符合泗河水文、水资源特征和水环境状况的河流水环境容量模型,与GIS技术结合构建了适合北方地区的河流水环境容量计算程序和方法;摸清了水功能区-入河排污口-点源排放口的一一对应关系,提出了将水域环境容量转换为陆域点源最大允许排污量的估算方法。计算了泗河在满足水功能区划条件下的水环境容量及最大允许排污量,从而为制定该河流水污染物容量总量控制方案提供了科学依据。     

环境管理手段对企业排污行为调控力度的定量化研究

在构造出反映企业排污行为和若干环境管理手段的统计特征量的基础上,提出以统计特征量之间的回归分析来定量化研究环境管理手段对企业排污行为调控力度的方法．对1993 ～1997年度镇江市26家COD 重点排放企业的研究表明：排污收费、环保补贴、执法检查、行政干预4 种环境管理手段都对企业的 COD 排放行为起到了明显的调控作用,调控力度由大到小依次为环保补贴、排污收费、执法检查和行政干预．     

隧道排污量估算与治污效果预测

通过隧道排污量和排污效果的简单分析,指出了其排污治理过程中应注意的有关事项,如进 行人口控制,改善居民的生活方式,提高环境保护意识和治理技术等,所述分析方法可供其它类似 工程参考。     

DBD低温等离子体气化杨木及模型化合物

本文利用低温等离子体技术,使用介质阻挡放电反应器气化杨木屑、纤维素、木聚糖和木质素,用控制变量法研究了频率、载气对反应系统产气能力的影响以及生物质化学组成的气化特性.结果表明,频率越小、载气电离能越低,气化率越高,杨木的最佳气化率为64.11％;木聚糖和纤维素气化产物相似,较纤维素和木质素产气率更高并且能够产生更多CO...     

Isotope tracing of submarine groundwater discharge offshore Ubatuba, Brazil: results of the IAEA–UNESCO SGD project

Results of groundwater and seawater analyses for radioactive (³H, ²²²Rn, ²²³Ra, ²²⁴Ra, ²²⁶Ra, and ²²⁸Ra) and stable (D and ¹⁸O) isotopes are presented together with in situ spatial mapping and time series ²²²Rn measurements in seawater, direct seepage measurements using manual and automated seepage meters, pore water investigations using different tracers and piezometric techniques, and geoelectric surveys probing the coast. This study represents first time that such a new complex arsenal of radioactive and non-radioactive tracer techniques and geophysical methods have been used for simultaneous submarine groundwater discharge (SGD) investigations. Large fluctuations of SGD fluxes were observed at sites situated only a few meters apart (from 0 cm d⁻¹ to 360 cm d⁻¹; the unit represents cm³/cm²/day), as well as during a few hours (from 0 cm d⁻¹ to 110 cm d⁻¹), strongly depending on the tidal fluctuations. The average SGD flux estimated from continuous ²²²Rn measurements is 17 ± 10 cm d⁻¹. Integrated coastal SGD flux estimated for the Ubatuba coast using radium isotopes is about 7 × 10³ m³ d⁻¹ per km of the coast. The isotopic composition (δD and δ¹⁸O) of submarine waters was characterised by significant variability and heavy isotope enrichment, indicating that the contribution of groundwater in submarine waters varied from a small percentage to 20%. However, this contribution with increasing offshore distance became negligible. Automated seepage meters and time series measurements of ²²²Rn activity concentration showed a negative correlation between the SGD rates and tidal stage. This is likely caused by sea level changes as tidal effects induce variations of hydraulic gradients. The geoelectric probing and piezometric measurements contributed to better understanding of the spatial distribution of different water masses present along the coast. The radium isotope data showed scattered distributions with offshore distance, which imply that seawater in a complex coast with many small bays and islands was influenced by local currents and groundwater/seawater mixing. This has also been confirmed by a relatively short residence time of 1–2 weeks for water within 25 km offshore, as obtained by short-lived radium isotopes. The irregular distribution of SGD seen at Ubatuba is a characteristic of fractured rock aquifers, fed by coastal groundwater and recirculated seawater with small admixtures of groundwater, which is of potential environmental concern and has implications on the management of freshwater resources in the region.     

乌江干流中上游水电梯级开发水温累积效应

以乌江流域洪家渡库尾至乌江渡坝下的水电工程干扰典型段为研究区域，利用建坝前后的水温实测资料，采用建坝前天然水温和建坝后下泄水温比较法，对乌江干流梯级水库水温时空分布特征进行分析。研究结果表明：对天然水温改变最大的电站为洪家渡和乌江渡，前者是受水库水温结构自身影响，后者是梯级联合运行的结果；梯级联合运行使库区水温分层有所减弱，随着时间的推移或上游梯级电站的建成，电站下泄水温年变化过程趋于均化，与天然水温的延迟也越加明显；不同的水库水温结构对水温累积效应的影响也各不相同，稳定分层型水库对水温累积具有正效应，混合型水库具有负效应，过渡型水库处于两者之间，体现了梯级电站的水温累积影响，为研究减缓下泄低温水的对策措施提供依据和参考。     

Local Area Quotas for Industrial Emissions along Reaches of the Pearl River in Guangdong

Abstract

There is an obvious departure from the regional equilibrium of developments between the upper and lower reaches of the Pearl River in Guangdong, which resulted in “the effects of contra-geography-grads development”. It is mainly because the upriver mountainous areas have been deeply stuck in industrialization delay and marginalization plights, so that nearly 40 million local people have conceived a dream to get rid of “the vicious circle of poverty” by speeding up industrial development. But the problem is that such industrialization efforts on a large scale in mountainous areas are encountering the bottleneck of environmental capacity that strictly limits industrial emissions along the upper reaches of any water system. As a solution, an institutional arrangement called “the Local Area Quotas for Industrial Emis-sions along the Pearl River” is put forward supposed to give corresponding compensation to the rights of industrial development yielded by some areas with lower environmental capacity through the distribution and trading of IDQs.