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）。     

基于改进的YOLOv4安全帽佩戴检测研究

为了加强建筑工人佩戴安全帽情况的检测,防止安全事故的发生,提出1种改进的轻量级YOLOv4安全帽佩戴检测算法,用于运行在移动设备端,降低现场部署的条件;制作1个8 000幅图像的数据集,用于训练和评估安全帽检测算法;为了评估改进的YOLOv4的性能,从5个不同建筑工地采集到600张施工人员图像和60条施工视频作为验证集;根据建筑工地不同的视觉条件对图像进行分类,用于验证本文算法在不同外界环境下的性能。结果表明:改进后的模型检测速度是YOLOv4的3.4倍,可用于实时检测施工人员在不同施工现场条件下是否佩戴安全帽的情况,有利于提高安全检查和监督水平。     

沼泽湿地植物光合特性及固“碳”潜势对外源氮输入的响应

以沼泽湿地典型草甸植被小叶章(Calamagrostis angustifolia)为研究对象,在三江平原进行了野外培养实验,探讨了4个不同氮素输入水平(0(NO)、6(N6),12(N12)、24(N24)g·m-2· a-1)下沼泽湿地植物生长与光合特性的响应特征,并从光合固"碳"的角度分析了小叶章沼泽湿地的固"碳"潜势.结果表明,外源氮输入明显促进了小叶章的株高、叶面积及植株数,显著增加了碳的生物量积累,到植物生长季结束,N6、N12和N24三个施氮水平下,小叶章地上部分生物量分别比对照增加了58.79%、133.11%和190.55%.同时,小叶章叶片全氮含量、叶绿素、可溶性蛋白和游离氨基酸含量也显著增加,净光合速率明显提高,分别比对照增加了20.70%、26.69%和53.54%.从光合固"碳"的角度来看,外源氮输入能够促使沼泽湿地植物通过光合作用固定更多CO2.     

Enhanced biological nutrient removal by the alliance of a heterotrophic nitrifying strain with a nitrogen removing ecosystem

Nitrogen removal from synthetic wastewater was investigated in an airlift bioreactor （ALB）, augmented with a novel heterotrophic nitrifier Pseudonocardia ammonioxydans H9^T under organic carbon to nitrogen ratios （Corg/N） ranging from 0 to 12. Effect of the inoculated strain was also determined on the settling properties and the removal of chemical oxygen demand （COD）. Two laboratory scale reactors were set up to achieve a stable nitrifying state under the same physicochemical conditions of hydraulic retention time （HRT）, temperature, pH and dissolved oxygen （DO）, and operated under the sequencing batch mode. The level of DO was kept at 0.5- 1.5 mg/L by periodic stirring and aeration. Each specific Corg/N ratio was continued for duration of 3 weeks. One of the reactors （BR2） was inoculated with P ammonioxydans H9^T periodically at the start of each Corg/N ratio. Sludge volumetric index （SVI） improved with the increasing Corg/N ratio, but no significant difference was detected between the two reactors. BR2 showed higher levels of nitrogen removal with the increasing heterotrophic conditions, and the ammonia removal reached to the level of 82%-88%, up to10% higher than that in the control reactor （BR1） at Corg/N ratios higher than 6; however, the ammonia removal level in experimental reactor was up to 8% lower than that in control reactor at Corg/N ratios lower than 2. The COD removal efficiency progressively increased with the increasing Corg/N ratios in both of the reactors. The COD removal percentage up to peak values of 88%-94% in BR2, up to 11% higher than that in BR1 at Corg/N ratio higher than 4. The peak values of ammonia and COD removal almost coincided with the highest number （18%-27% to total bacterial number） of the exogenous bacterium in the BR2, detected as colony forming units （CFU）. Furthermore, the removal of ammonia and COD in BR2 was closely related to the number of the inoculated strain with a coefficient index （R2） up to 0.82 and 0.85 for ammonia and     

水样中挥发酚测定的边界条件探讨

在环境水质监测中,水中挥发酚的测定是最重要的有机监测项目。水样测定中首选测定方法是4-氨基安替比林光度法。在水样预处理和分析操作过程中,既要严格执行操作技术规程,更要充分考虑分析过程中的关键技术、边界条件等一些因素的影响,特别要考虑4-氨基安替比林的空白值、显色剂的稳定性、pH值的影响及缓冲液的使用等以保证实验的顺利进行和分析数据真实准确有效。     

一种改性柱撑蒙脱石的制备及其对废水中SO2-4吸附效率研究

蒙脱石具有较大的比表面积和阳离子交换容量,吸附性能较好.但其不能有效地吸附疏水性物质,应用中常将一些聚合羟基金属阳离子引入到蒙脱石层间制成柱撑蒙脱石以提高其孔道特性和热稳定性.为了进一步提高其吸附效率,在柱撑蒙脱石中加入了物料A,高温焙烧,对其进行了一系列的改性,并确定了改性条件,制备了一种新型的SO2-4高效吸附剂,并应用于煤矿矿井废水的治理,改性后的吸附剂较柱撑蒙脱石对水中SO2-4的吸附率提高了54.6%.最佳焙烧温度为800℃,焙烧时间为4 h,焙烧的最佳物料配比为1:4.     

水中挥发酚检测方法初探

酚类属高毒物质,水中挥发酚的含量直接影响人类健康。近10年来,我国研究人员对水中挥发酚的测定方法开展了很多研究,特别对于采用4-氨基安替比林分光光度法(4-AAP)(GB 7490-1987)测定水中挥发酚的各个环节,如样品的采集、保存、预处理、试剂纯度、反应时间控制等相关因素进行了研究,找到了影响含量准确的因素,为测定水中挥发酚的含量提供了快速、准确、重复性好的方法。对一些非国标法测定水中挥发酚的方法也进行了介绍。文章对这些方法进行了分类总结。希望能对实验人员有所帮助。     

氮沉降对陆地生态系统土壤有机碳含量影响的Meta分析

研究已证实大气氮沉降的增加显著影响了土壤有机碳的含量,然而其变化幅度在不同的实验样地具有较大的差异.基于在我国开展的49个模拟氮沉降野外实验的408组数据,利用Meta分析、Meta回归和线性回归等方法系统研究了样地气候、土壤属性以及氮素施用参数对施氮后土壤有机碳含量的影响.结果表明,样地的年均温（MAT）和年均降水量（MAP）与施氮后土壤有机碳含量变化幅度显著正相关（P<0.05）.在MAT或MAP较低（MAT<3℃,MAP<500 mm）的样地中,施氮后土壤有机碳含量显著下降;而在MAT或MAP较高（MAT>3℃,MAP>500 mm）的样地中,施氮后土壤有机碳含量则显著升高.土壤属性方面,在C：N较高（>15）或酸性（pH<6.5）土壤中,施氮后土壤有机碳积累明显（P<0.05）;而在C：N较低（≤15）以及中性或碱性（pH≥6.5）土壤中,施氮后土壤有机碳变化不明显（P >0.05）.此外,施氮后草原生态系统土壤有机碳含量明显下降（-5.34%）;而湿地生态系统土壤有机碳含量变化不明显;森林生态系统土壤有机碳表现出明显积累（10.52%）,特别是阔叶林生态系统（13.10%）.所有的因子中,土壤C：N是影响施氮后土壤有机碳变化幅度的主导因子.在施氮类型方面,施加硝酸铵或尿素后土壤有机碳含量显著升高,而施加硝态氮对其影响不显著.综上所述,在精确评估、预测和分析氮沉降对土壤有机碳含量的影响时,应综合考虑样地的气候、土壤属性以及氮素施用参数等因素对实验结果的影响.     

MTBE装置潜在危险性分析及物料泄漏扩散后果模拟研究

MTBE装置处理的物料（混合C4、甲醇）具有易燃易爆性,若发生物料泄漏,将导致装置发生火灾爆炸。为了确保装置安全平稳、长周期运行,基于MTBE装置工艺技术特点,全面系统分析了装置的潜在危险性,总结出导致装置发生火灾爆炸事故的主要因素-物料泄漏;在此基础上,采用挪威DNV公司的SAFETI定量风险评价软件,建立混合C4、甲醇泄漏扩散模型,对物料泄漏导致的主要事故类型（喷射火、池火等）进行模拟,得出泄漏扩散引发火灾爆炸事故的危害范围。结果表明：该模拟研究能够反映出泄漏扩散过程和破坏范围,取得了较真实的事故影响范围曲线图,可以为设计人员更加详细了解MTBE装置发生事故的危害性及企业加强重点部位监控、制定防范措施、编制事故应急预案提供重要参考依据。     

Integrating soil carbon cycling with that of nitrogen and phosphorus in the watershed model SWAT: Theory and model testing

In this paper we describe and test a sub-model that integrates the cycling of carbon (C), nitrogen (N) and phosphorus (P) in the Soil Water Assessment Tool (SWAT) watershed model. The core of the sub-model is a multi-layer, one-pool soil organic carbon (S_C) algorithm, in which the decomposition rate of S_C and input rate to S_C (through decomposition and humification of residues) depend on the current size of S_C. The organic N and P fluxes are coupled to that of C and depend on the available mineral N and P, and the C:N and N:P ratios of the decomposing pools. Tillage explicitly affects the soil organic matter turnover rate through tool-specific coefficients. Unlike most models, the turnover of soil organic matter does not follow first order kinetics. Each soil layer has a specific maximum capacity to accumulate C or C saturation (S_x) that depends on texture and controls the turnover rate. It is shown in an analytical solution that S_x is a parameter with major influence in the model C dynamics. Testing with a 65-yr data set from the dryland wheat growing region in Oregon shows that the model adequately simulates the S_C dynamics in the topsoil (top 0.3 m) for three different treatments. Three key model parameters, the optimal decomposition and humification rates and a factor controlling the effect of soil moisture and temperature on the decomposition rate, showed low uncertainty as determined by generalized likelihood uncertainty estimation. Nonetheless, the parameter set that provided accurate simulations in the topsoil tended to overestimate S_C in the subsoil, suggesting that a mechanism that expresses at depth might not be represented in the current sub-model structure. The explicit integration of C, N, and P fluxes allows for a more cohesive simulation of nutrient cycling in the SWAT model. The sub-model has to be tested in forestland and rangeland in addition to agricultural land, and in diverse soils with extreme properties such high or low pH, an organic horizon, or volcanic soils.