交替冻融对东北地区典型土壤氮磷浓度的影响

研究了交替冻融对东北地区黑土、暗棕壤和水稻土中的全氮、有效氮、全磷和有效磷的影响。结果表明,经过15次交替冻融后,三种类型土壤的全氮浓度均未发生明显变化,说明在交替冻融过程中,硝化与反硝化共同作用并不明显。由于冻融作用增强土壤释水性和水分渗透性,经15次交替冻融后,黑土、暗棕壤和水稻土的有效氮浓度均有所升高,以水稻土最显著,上升了31.25%。三种土壤全磷浓度均在初次冻融后大幅增高,总体呈升高趋势,分析原因主要是冻融作用破坏了土壤团聚体,增加了与消化液反应的机会。经15次交替冻融后,黑土和水稻土的有效磷浓度分别上升17.72%和56.16%,暗棕壤的有效磷浓度下降35.19%,这说明交替冻融过程中土壤有效磷的变化不但取决于土壤的C/P,还受土地利用类型的影响,林地的有效磷浓度可能由于发生磷的净固定而降低。     

规模化养猪场生命周期环境影响评价

利用生命周期评价(LCA)方法建立规模化养猪场系统能源消耗和污染物排放清单,对系统生命周期不同阶段环境影响进行评价,通过评价找出降低环境影响的方法。研究了四个环境影响类型：能源消耗、富营养化、全球变暖和环境酸化,得出各类型环境影响指数分别为8.38×10^-3,1.91×10^-3,9.80×10^-3和2.01×10^-2;将系统生命周期分成饲料原料生产、生猪饲养和废物处理三个环节,得出各环节环境影响综合指数分别为2.52×10^-2,1.23×10^-2和2.71×10^-3。结果表明,饲料原料生产环节的环境影响最大,因此,减少氮肥的使用量并在生产过程中实施节能和清洁生产,是控制规模化养猪场生命周期环境影响的关键。     

岩溶地区土壤溶解有机碳的季节动态及环境效应

对桂林岩溶试验场土壤溶解有机碳(DOC)进行了逐月的观测，结果显示DOC是岩溶生态系统中活跃的有机碳组分，在岩溶地区碳循环中发挥着重要的作用。一年中土壤DOC的变化特征表现为3个阶段：(1)3-7月，随气温升高、降雨量增加，土壤生物活性和新陈代谢能力极大提高，土壤溶解有机碳呈升高趋势；(2)8-11月，气温保持较高的水平，但降雨量偏低，土壤干燥，土壤微生物活性极大地减弱，土壤DOC质量分数全年最低；(3)12月至次年2月，随温度的降低，土壤生物活性逐渐降低，土壤DOC呈缓慢升高趋势，且与土壤微生物量碳之间存在互为消长的关系。土壤碳酸盐岩的溶蚀速率季节变化与土壤DOC之间存在负相关。文章还提出了岩溶地区土壤碳循环模式及DOC在其中的作用。     

Seaweed sex pheromones and their degradation products frequently suppress amphipod feeding but rarely suppress sea urchin feeding

Summary. A diverse group of brown seaweeds produce bouquets of C₁₁ metabolites, some of which act as pheromones that cue gamete release or attract sperm to eggs following release. We demonstrate that these C₁₁ metabolites and their degradation products also frequently and strongly deter feeding by the herbivorous amphipod Ampithoe longimana, but rarely by the herbivorous sea urchin Arbacia punctulata. Across the range of concentrations tested, seven of twelve C₁₁ metabolites or mixtures that we tested deterred feeding by the amphipod, but only two of eleven deterred the sea urchin. For those compounds where we could rigorously contrast the magnitude of deterrence against the amphipod with the magnitude of deterrence against the urchin, the amphipod was deterred significantly more than the urchin by five of six metabolites. Thus, C₁₁ compounds were more frequently and more strongly deterrent to the amphipod than to the sea urchin. These findings for C₁₁ metabolites conflict with previous investigations, where other classes of seaweed chemical defenses have been shown to deter feeding by large mobile herbivores like urchins and fishes but to be relatively ineffective against mesograzers, especially the species of amphipod that we used here. Our results suggest that C₁₁ metabolites are unusual among the known seaweed chemical defenses in that they are especially effective against mesograzers, which often consume seaweed spores, zygotes, and juveniles. The high concentrations of C₁₁ metabolites in brown algal eggs could allow these defenses to be especially important in defending gametes, zygotes, or young sporelings from herbivorous mesograzers. Received 26 February 1998; accepted 9 April 1998.     

基于DNDC模型评估水位变化对滨海湿地净生态系统CO2交换的影响

水位是影响滨海湿地生态系统蓝碳功能的重要因素。气候变化引起的海平面上升以及极端气候事件的频发,可能加快水位的变化,从而改变生态系统碳交换的过程。然而,滨海湿地碳汇功能响应水位变化的机制尚不清楚。为了评估水位对滨海湿地净生态系统CO₂交换(NEE)特征的影响,以及验证DNDC(denitrification-decomposition)模型对模拟预测滨海湿地生态系统碳交换的适用性,该研究设计了野外水位控制试验(自然水位,地下20 cm水位、地表10 cm水位),并利用DNDC模型模拟和预测水位变化对滨海湿地NEE的影响。结果表明:(1)不同水位处理之间NEE差异显著,地表10 cm水位处理促进CO₂吸收,地下20 cm水位则抑制CO₂吸收;(2)经过校准和验证的DNDC模型可以准确模拟水位变化对黄河三角洲湿地NEE的影响,NEE模拟值的日动态与田间观测结果显著相关(R²>0.6);(3)通过改变气候、土壤和田间管理等输入参数对DNDC模型进行灵敏度检验,生态系统碳交换过程对日均温、降雨和水位改变的响应最为显著,其中,水位对NEE的影响主要作用于土壤呼吸(Rs)。未来气候情境下,不同水位变化下的生态系统碳交换过程随年份增长呈现不同的规律,因此未来的模拟研究应关注DNDC中水文模块和植被演替过程的完善。该研究可为预测水文变化情境下滨海湿地碳汇功能的未来发展以及政策制定提供参考。     

珠江流域土壤中碳库的存量与通量

通过对珠江流域各主要环境介质中不同形态碳含量的分析和计算,得出该流域0~1.0m范围内土壤碳库的存量为1.36×1013kg,占中国陆地碳库总量的9.51%,全球碳库总量的0.907%;流域净碳输入量为4.141×1010kg/a,碳通量912.74kg/(hm2·a),初步计算表明珠江流域可能是陆地生态系统的一个碳汇区。另一方面,人类活动造成流域内有机碳的大量流失,其中,水土流失损失的碳8.01×109kg/a,植物收割及森林砍伐从土壤-植物系统中携带出的有机碳高达6.26×1011kg/a,这将造成土壤有机质含量的降低,因此促进陆地生态系统有机碳存储是提高本流域土地质量的关键。     

生活垃圾堆肥工艺条件及其反应动力学研究

为了改善堆肥微环境 ,提高生活垃圾堆肥速率 ,研究堆肥工艺条件及其反应动力学是非常必要的。通过控制堆肥工艺条件 ,如初始温度、含水率、C/N比及堆料颗粒大小 ,研究生活垃圾堆肥过程中生物、化学及物理因素的变化。试验结果表明 ,生活垃圾堆肥反应符合一级反应动力学 ;合理控制堆肥初始反应条件 ,能明显提高堆肥效率。     

碳氮比对低温投加介体生物反硝化脱氮的影响

污水的生物脱氮效果受低温抑制,投加氧化还原介体有利于反硝化过程。采用规格相同的序批式反应器,使用人工配制硝酸盐废水和经过驯化的活性污泥,考察了不同碳源浓度(碳氮比)对低温(10 ℃)投加氧化还原介体1, 2-萘醌-4-磺酸(NQS)污水生物反硝化脱氮过程的影响。结果表明：当碳源浓度(以COD计)为150~400 mg·L⁻¹ (碳氮比为1.8~4.7)时,脱氮效率随碳氮比的升高而升高;当碳源浓度为400~550 mg·L⁻¹ (碳氮比为4.7~6.5)时,脱氮效率随着碳氮比的升高而降低;当碳源浓度为400 mg·L⁻¹ (碳氮比为4.7)左右时效果最好,总氮去除率最高为64.7%。对于脱氮速率,介体强化脱氮速率随着碳氮比的升高而升高。同时,探讨了投加介体污水生物反硝化脱氮的机理,发现投加介体降低了体系的氧化还原电位(ORP),有利于反硝化脱氮反应的进行。     

染整废水处理工程设计

采用“生物接触氧化 +混凝气浮 +生物炭”工艺处理染整废水 ,COD去除率可达到 90 %以上 ,工程实践表明 ,该工艺处理效果好 ,运行稳定 ,投资省 ,处理后出水可达标排放     

Influence of pore structure on biologically activated carbon performance and biofilm microbial characteristics

• Pore structure affects biologically activated carbon performance. • Pore structure determines organic matter (OM) removal mechanism. • Microbial community structure is related to pore structure and OM removal. Optimizing the characteristics of granular activated carbon (GAC) can improve the performance of biologically activated carbon (BAC) filters, and iodine value has always been the principal index for GAC selection. However, in this study, among three types of GAC treating the same humic acid-contaminated water, one had an iodine value 35% lower than the other two, but the dissolved organic carbon removal efficiency of its BAC was less than 5% away from the others. Iodine value was found to influence the removal of different organic fractions instead of the total removal efficiency. Based on the removal and biological characteristics, two possible mechanisms of organic matter removal during steady-state were suggested. For GAC with poor micropore volume and iodine value, high molecular weight substances (3500–9000 Da) were removed mainly through degradation by microorganisms, and the biodegraded organics (soluble microbial by-products,<3500 Da) were released because of the low adsorption capacity of activated carbon. For GAC with higher micropore volume and iodine value, organics with low molecular weight (<3500 Da) were more easily removed, first being adsorbed by micropores and then biodegraded by the biofilm. The biomass was determined by the pore volume with pore diameters greater than 100 μm, but did not correspond to the removal efficiency. Nevertheless, the microbial community structure was coordinate with both the pore structure and the organic removal characteristics. The findings provide a theoretical basis for selecting GAC for the BAC process based on its pore structure.