草地退化对三江源区高寒草甸生态系统CO2通量的影响及其原因

为了揭示草地退化对三江源地区高寒草甸生态系统碳通量的影响,利用涡度相关技术,于2006年12月1日~2007年11月30日对三江源地区的退化高寒草甸生态系统的碳通量及生物和环境因子进行观测.结果发现:草地退化对高寒草甸生态系统的碳通量产生了深刻影响,与未退化的高寒草甸生态系统相比,退化高寒草甸生态系统全年总初级生产力(GPP)下降了36.6%,全年生态系统呼吸(Reco)下降了7.9%,全年净生态系统CO2交换(NEE)也由退化前的负值(碳吸收)转变为正值(碳排放),二者相差132.5gC/(m2·a),生态系统由原来的碳汇转变为目前的碳源.这些变化与高寒草甸退化后,生态系统植物地上生物量锐减、植物生长期缩短(NEE<0的天数)、植物多样性下降、土壤含水量降低等因素密切相关.     

我国电解锰行业氨氮污染分析与控制

我国"十二五"期间将氨氮纳入总量控制指标,电解锰行业氨氮污染控制变得非常紧迫。介绍了电解锰氨氮污染的现状,分析了电解锰氨氮污染的产生途径以及电解锰生产中的氨氮平衡,依据"源头消减、过程控制、末端循环"的清洁生产理念,提出了电解锰氨氮污染的控制措施。     

Effect of iron addition on the performance of anoxic-oxic membrane process and biological phosphorus removal北大核心CSCD

In order to solve the problem of poor treatment of phosphorus in membrane bioreactor (MBR) with long sludge retention time (SRT), a ferric salt was added to enhance phosphorus removal; FeCl36H2O (Fe/P = 2.0) was added to the reactor. The removal efficiency of nitrogen, organic matters, and phosphorus in the MBR was investigated systematically. Moreover, this study focused on the membrane performance, the change of active sludge flora, and the effect of adding a ferric salt on membrane fouling before and after the addition. It was seen that adding the ferric salt could not affect the removal of COD and NH4 +-N and the removal rate of COD and NH4 +-N reached over 90%. However, the average removal rate of phosphorus was 52%, while the removal rate increased by nearly 40% after adding the ferric salt. The effects of adding ferric salts on the dominant bacteria and biological phosphorus removal of activated sludge were further studied. The results showed that the addition of ferric salt (Fe/P = 2.0) decreased the diversity of active sludge flora and relative abundance of some phosphorusaccumulating organisms and had a negative effect on biological phosphorus removal. The analysis of transmembrane pressure difference (TMP) recording revealed that the concentration of iron salts did not exacerbate membrane fouling. The results showed that the concentration of iron salts entering the membrane bioreactor would reduce the relative abundance and phosphorus removal efficiency of the activated sludge in the system to a certain extent, but it had no obvious effect on membrane fouling. It allowed the effluent to attain acceptable standards, especially with respect to phosphorus removal efficiency. © 2018 Science Press. All rights reserved.     

海洋平台井喷含硫天然气扩散危险区域研究

针对海洋酸性气田开采过程中含硫天然气井喷失控扩散问题,采用CFD方法建立井喷含硫天然气扩散后果预测与评估模型。综合考虑天然气爆燃与硫化氢毒害风险因素,对不同场景条件下的含硫天然气扩散过程开展数值模拟,研究硫化氢浓度、风向、风速等因素对含硫天然气扩散行为的影响,预测和评估天然气扩散所形成的危险区域和硫化氢气体扩散所形成的毒害范围。研究表明:随着硫化氢浓度的增加,燃爆区域无明显变化,而毒害区域明显增加;船艉来风导致的事故后果最为严重,左、右舷来风有利于危险气体的扩散与消散;风速越大,燃爆区域和毒害区域范围越小,但是在船艏来风且风速较大的工况下,硫化氢气体竖直扩散距离降低且逐渐贴近生活区,容易造成作业人员中毒事故的发生。     

污泥填埋场气体产量的预测方法研究

为有效利用污泥填埋场内产生的沼气,以上海白龙港污水处理厂污泥为例,对污泥填埋场中气体产生率及产生量进行了预测.应用元素的归一化摩尔化方法得到该污水处理厂污泥有机物的近似分子式为C28H52O16N4.用化学计量法和IPCC模型预测的甲烷气体产生潜能分别为60.6,61.7kg/t(以干重计).用动力学模型和IPCC模型预测的甲烷气体产生率分别为13.3,11.1kg/(t×a)(以干重计),2种方法计算的甲烷气体产生率的差别主要在于参数的取值不同,化学计量法和动力学模型法预测的气体产生量和产生率更能反映污泥填埋场实际的气体产生情况,应用IPCC模型更适合于从宏观角度估算一个地区或整个国家的填埋场产气量.     

含固率和接种比对林可霉素菌渣厌氧消化的影响

通过林可霉素菌渣的中温厌氧消化摇瓶实验,比较不同的含固率(3%、5%、8%、10%)和接种比(0.5、1、2、3)对菌渣产甲烷能力的影响,以确定菌渣厌氧消化的最优工艺条件.结果表明,在研究参数范围内,含固率越低,接种比越高,越有利于甲烷的产生;经过10d的培养,在含固率为3%、接种比为3时的工况中,菌渣的挥发性固体(VS)累计净产甲烷量最高,为106 mL/g;而含固率>5%、接种比2的液态发酵工艺,此条件既能保证厌氧消化不受消化产物(胺和挥发性有机酸)积累的抑制,也可以缓冲菌渣中残留林可霉素对消化微生物可能产生的抑制效应.     

应用呼吸-滴定测量监测硝化动态过程

将pH值在线监测与药品自动投加系统与已开发的混合呼吸测量仪集成,组成自动呼吸-滴定测量仪,同时测定废水生物处理过程氧气利用速率(OUR)和质子变化速率(HVR).对活性污泥硝化过程定时测定NH4+-N浓度,比较其与基于HVR或OUR预测的NH4+-N浓度间的一致程度,评估自动滴定测量装置测试硝化过程动态的性能.结果表明,在初始NH4+-N浓度分别为20,25mg/L的间歇试验中,实测值数组与基于OUR的预测值数组间的相关系数分别为0.9967和0.9972,与基于HVR的预测值数组间的相关系数分别为0.9991和0.9992,表明OUR和HVR均能及时准确地反映硝化过程的动态特性.     

Tradeoffs between forestry resource and conservation values under alternate policy regimes: A spatial analysis of the western Canadian boreal plains

An important element of resource management and conservation is an understanding of the tradeoffs between marketed products, such as timber, and measures of environmental quality, such as biodiversity. In this paper, we develop an integrated economic-ecological spatial optimization model that we then apply to evaluate alternate forest policies on a 560,000 km² study region of managed boreal forest in Alberta and British Columbia, Canada. The integrated model incorporates dynamic forest sector harvesting, current levels of oil and gas sector development, coarse-filter or habitat-based old forest indicators, a set of empirical forest bird abundance models, and statistical models of the natural and current fire regimes. Using our integrated model, economic tradeoff curves, or production possibility frontiers, are developed to illustrate the cost of achieving coarse-filter targets by a set time (50 years) within a 100-year time horizon. We found levels of ecological indicators and economic returns from the timber industry could both be increased if spatial constraints imposed by the current policy environment were relaxed; other factors being equal, this implies current policy should be revised. We explore the production possibility frontier's relationship to the range of natural variation of old forest habitat, and show how this range can be used to guide choices of preferred locations along the frontier. We also show that coarse-filter constraints on the abundance of certain habitat elements are sufficient to satisfy some fine-filter objectives, expressed as the predicted abundances of various species of songbirds.     

冬季土地管理对稻季CH4产生、氧化和排放的影响

通过室内培养和田间试验测定了冬季休闲、种麦和淹水处理水稻生长期CH4的产生潜力、氧化潜力及其排放通量,以探讨冬季土地管理对后续稻季CH4产生、氧化和排放的影响。结果表明：休闲与种麦处理间CH4产生潜力无显著差异（P〉0．05）,但2者均显著低于淹水处理（P〈0．05）;各处理间CH4氧化潜力无显著差异（P〉0．05）,土壤中NH4^＋-N含量可能是较冬季土地管理更为重要的影响CH4氧化潜力的因素;休闲处理CH4平均排放通量显著高于种麦处理（P〈0．05）,但2者均显著低于淹水处理（P〈0．05）。冬季持续淹水稻田CH4产生潜力显著高于冬季排水稻田是其CH4排放量远高于冬季排水稻田的原因。冬季土地管理对稻季CH4排放的影响主要受CH4产生潜力而非CH4氧化潜力的限制。     

冬季淹水稻田CH_4产生、氧化和排放规律及其影响因素研究

采用静态箱/气象色谱法——田间原位观测和室内培养试验连续一年研究了冬季淹水稻田的CH4产生潜力、氧化潜力和排放通量,以探讨冬季淹水稻田CH4产生、氧化和排放的季节变化规律及其影响因素。结果表明：0~251 d（d表示淹水后天数）,CH4产生潜力逐渐增大,到251 d达最大值,之后逐渐减小;0~204 d,CH4氧化潜力变化较小,但到235 d急剧增至最大值,随后逐渐减小;0~169 d,稻田几乎没有CH4排放,192 d才开始有较明显的CH4排放,到230 d达最大值,为80.2 mg.m-2.h-1,随后逐渐减小,331 d出现一个CH4排放高峰。全观测期内CH4排放量为69.9 g.m-2,其中非水稻生长期排放6.7 g.m-2,占总量的9.5%。全观测期内CH4产生潜力与土温及土壤Eh均无显著相关性;全观测期内CH4氧化潜力与土温极显著正相关（P〈0.01）,水稻生长期CH4氧化潜力与土壤中氨氮含量呈极显著正相关（P〈0.01）;全观测期内稻田CH4排放与土温和CH4产生潜力两个因素均显著正相关（P〈0.05）而与土壤Eh呈显著负相关（P〈0.05）。