Simulating soil organic matter with CQESTR (v. 2.0): Model description and validation against long-term experiments across North America

Soil carbon (C) models are important tools for examining complex interactions between climate, crop and soil management practices, and to evaluate the long-term effects of management practices on C-storage potential in soils. CQESTR is a process-based carbon balance model that relates crop residue additions and crop and soil management to soil organic matter (SOM) accretion or loss. This model was developed for national use in U.S and calibrated initially in the Pacific Northwest. Our objectives were: (i) to revise the model, making it more applicable for wider geographic areas including potential international application, by modifying the thermal effect and incorporating soil texture and drainage effects, and (ii) to recalibrate and validate it for an extended range of soil properties and climate conditions. The current version of CQESTR (v. 2.0) is presented with the algorithms necessary to simulate SOM at field scale. Input data for SOM calculation include crop rotation, aboveground and belowground biomass additions, tillage, weather, and the nitrogen content of crop residues and any organic amendments. The model was validated with long-term data from across North America. Regression analysis of 306 pairs of predicted and measured SOM data under diverse climate, soil texture and drainage classes, and agronomic practices at 13 agricultural sites having a range of SOM (7.3–57.9 g SOM kg⁻¹), resulted in a linear relationship with an r² of 0.95 (P < 0.0001) and a 95% confidence interval of 4.3 g SOM kg⁻¹. Using the same data the version 1.0 of CQESTR had an r² of 0.71 with a 95% confidence interval of 5.5 g SOM kg⁻¹. The model can be used as a tool to predict and evaluate SOM changes from various management practices and offers the potential to estimate C accretion required for C credits.     

一体化膜生物反应器处理低C/N污水试验研究

研究一体化连续流间歇曝气膜生物反应器(IMBR)处理低C/N城市污水的工艺效能。试验结果表明:反应器在曝气2 h、搅拌2 h的运行模式下,对COD、NH4+-N、TN和SS的平均去除率分别达到了87%,83.4%,75.4%和97.81%,各出水质量浓度平均值分别为17.5,4.59,7.63和2 mg/L,出水水质达到了GB/T18920-2002《城市污水再生利用城市杂用水水质》标准。     

(Z)-Dodec-3-en-1-ol, a common major component of the trail-following pheromone in the termites Kalotermitidae

(Z)-Dodec-3-en-1-ol has been identified as the major component of the trail-following pheromone of nine species of Kalotermitidae belonging to six different genera, suggesting that this compound represents a common signal in this family of termites. The homogeneous nature of trail-following pheromones of Kalotermitidae well agrees with the monophyly of this family. It also supports the postulated position of this family as a sister group of the Rhinotermitidae and Termitidae, which also secrete C12-alcohols as trail-following pheromones. The significance of a trail pheromone in termites of the ‘one-piece’ life type, which spend their whole life within the same piece of wood, is discussed.     

不同C/N值下亚硝酸盐氧化菌和异养菌混合体系的微生物多样性

采用PCR-RFLP技术研究了不同C/N比下亚硝酸盐氧化菌及异养菌混合体系的微牛物多样性,并探讨了微生物菌群结构与其功能(硝化件能)的关系.C/N=0时,混合体系主要由自养菌和寡营养菌(85.1%)组成,包括亚硝酸盐氧化菌(NOB)、拟杆菌门、α-变形菌纲、浮霉菌门和绿色非硫细菌中的一些菌株.C/N=0.44时,混合体系中的自养菌减少,异养菌(主要是γ-变形菌纲的成员)大量出现.C/N=8.82时,γ-变形菌纲的菌株尤其是反硝化菌Pseudomonas sp.占主导(93.8%),与此同时,随着C/N升高,该混合体系的硝化性能也由专一的亚硝酸盐氧化过程转变为同时硝化反硝化过程.微生物菌群结构的转变较好地解释了其硝化性能的改变.本研究揭示了微生物菌群结构与其功能的内在联系,同时表明PCR-RFLP技术与化学分析相结合是研究微生物菌群结构与功能的有力工具.图3表2参13     

环境安全：21世纪人类面临的根本问题

本文从人类社会的可持续进步和国家的可持续发展两个层面,深层次地分析了环境安全问题的不可替代的重要性,并从理论和实践两个方面得出：第一,我国应将环境安全的保证能力作为综合国力的重要组成部分;第二,应将环境安全观作为指导我国21世纪两大战略-加入WTO和西部大开发的重要方针。     

不同环境条件下偶氮染料酸性大红GR的生物降解性能

为了考察不同环境条件下偶氮染料酸性大红GR生物降解性能,采用已驯化的混合菌群作为接种液进行偶氮染料酸性大红GR脱色试验。结果表明,微氧条件下(静置敞口培养),偶氮染料酸性大红GR脱色效果最佳,染料脱色主要发生在菌体的对数生长期。混合菌群对pH、温度适应范围较广,pH为3.32~9.18,温度在20℃~37℃范围内均可以获得较好脱色效果,脱色率均在80%以上。微氧条件下酸性大红GR降解历程表明,偶氮基整个共轭系统被破坏,生成了一种新的结构,使原有的某些精细结构在二阶导数光谱中得以表现,由此探讨其生物降解机理。     

基于STC12C5410AD的电铃无线控制系统

针对传统电铃采用单一作息时间表进行专线控制的缺点,设计了一种能无线控制、又能同时存储多个作息时间表的电铃控制系统．该系统用无线代替专线,存储有多个时间表,在季节变更时通过控制器自动变换表,解决了传统电铃控制系统中的专线成本高、维修难、季节变换需要人工改表的问题．图5,表2,参4．     

碳氮比对分段进水生物脱氮的影响

探讨了6组不同的碳氮比(C/N)对分段进水生物脱氮工艺中进水流量分配、每一段中缺氧区好氧区容积比以及脱氮效率的影响.将进水总氮浓度恒定为42mg/L(凯氏氮浓度为40mg/L),以比较出水总氮浓度.结果表明,在一定C/N条件下,通过调整进水流量分配和每一段缺氧区与好氧区容积比可达到高于95%的总氮去除率.同时污泥体积指数也会随着进水流量分配系数的升高而增大.出水总氮浓度主要是由进水流量分配所决定,每一段中缺氧区好氧区的容积比影响不大.     

C9-AA水溶性石油树脂的制备及其阻垢性能

以乙烯生产过程中的副产物C9馏分和丙烯酸为原料,采用自由基溶液聚合,合成具有阻垢性能的C9-AA水溶性石油树脂。考察了引发剂AIBN和溶剂的加入量、C9-AA加入量、Ca^2＋浓度、循环冷却水pH和养护时间对C9-AA水溶性石油树脂阻垢性能的影响,并对其阻垢效果进行了评价。在Ca^2＋质量浓度小于或等于600mg／L、循环冷却水pH小于或等于9．3、C9-AA水溶性石油树脂加入量大于或等于15mg／L的条件下,C9—AA水溶性石油树脂对循环冷却水的阻垢率达到90％以上,其有效作用时间为60h。     

贵州梵净山九龙池沉积物14C年代学研究及全新世碳累积速率变化

放射性碳同位素加速器质谱(ASM¹⁴C)测年法是湖泊沉积物定年的主要方法,并且是全新世年代学研究的热点。随着对全新世古气候与环境变化研究的深入,选取不同介质定年可能对年代模型的准确性造成误差,进而影响到气候指标的解译。本文选取贵州东北部梵净山九龙池沉积物中树枝、树叶、树皮、种子等植物残体和全样有机质作为测年介质,利用ASM¹⁴C进行定年。结果表明,相比全样有机质,使用植物残体定年可以在一定程度上避免碳库效应的影响。但相比于原位沉积且生长年限较短的叶片,树枝的定年结果偏老,不是一种理想的定年介质。另外,根据定年结果及总有机碳含量重建了全新世九龙池的碳累积速率,发现碳累积速率可以指示该地区亚洲夏季风强度的变化历史。