Effect of fertilizer and water content on N2O emission from three plantation soils in South China

Introduction Nitrousoxide(N2O)isoneofthemostimportantgreen housegases,whichcontributestoglobalwarmingand consumptionofO3inthestratosphere(Breuer,2000,Solomon,1999).N2Oconcentrationincreasesatarateof0.25%peryear,57%ofwhichisderivedfromthesoildue tonitrific…     

Changes in visibility with PM2.5 composition and relative humidity at a background site in the Pearl River Delta region

In fall–winter, 2007–2013, visibility and light scattering coefficients(b sp) were measured along with PM_(2.5)mass concentrations and chemical compositions at a background site in the Pearl River Delta(PRD) region. The daily average visibility increased significantly(p 0.01) at a rate of 1.1 km/year, yet its median stabilized at ~13 km. No haze days occurred when the 24-hr mean PM_(2.5)mass concentration was below 75 μg/m~3. By multiple linear regression on the chemical budget of particle scattering coefficient(b sp), we obtained site-specific mass scattering efficiency(MSE) values of 6.5 ± 0.2, 2.6 ± 0.3, 2.4 ± 0.7 and 7.3 ± 1.2 m2/g,respectively, for organic matter(OM), ammonium sulfate(AS), ammonium nitrate(AN) and sea salt(SS). The reconstructed light extinction coefficient(b ext) based on the Interagency Monitoring of Protected Visual Environments(IMPROVE) algorithm with our site-specific MSE revealed that OM, AS, AN, SS and light-absorbing carbon(LAC) on average contributed 45.9% ± 1.6%,25.6% ± 1.2%, 12.0% ± 0.7%, 11.2% ± 0.9% and 5.4% ± 0.3% to light extinction, respectively.Averaged b ext displayed a significant reduction rate of 14.1/Mm·year(p 0.05); this rate would be 82% higher if it were not counteracted by increasing relative humidity(RH) and hygroscopic growth factor(f(RH)) at rates of 2.5% and 0.16/year-1(p 0.01), respectively, during the fall–winter, 2007–2013. This growth of RH and f(RH) partly offsets the positive effects of lowered AS in improving visibility, and aggravated the negative effects of increasing AN to impair visibility.     

解磷微生物对煤系废弃物粉煤灰的改良效应

燃煤产生大量的粉煤灰虽会严重污染环境,但却含有植物生长必需的营养元素,将其资源化生物利用是一条很好的途径.从粉煤灰和农田土壤中分离筛选出 2 株解磷细菌 CA 和 SL,以紫花苜蓿为供试植物,通过盆栽试验研究接种解磷细菌对粉煤灰基质的改良作用.研究表明,加入解磷细菌后,对粉煤灰基质有一定的改良作用,促进了植物生长,增加了对粉煤灰中难溶性磷的吸收利用,降低了粉煤灰 pH,增加了根际细菌和真菌的数量.从粉煤灰中筛选分离出的菌株 CA的改良作用更显著,苜蓿的地上干重比对照提高了45.1%.解磷微生物的应用对于实现废弃物粉煤灰场的生态恢复提供了新的技术与潜力.     

吸收塔溢流现象产生的原因及其控制措施

在湿式石灰石-石膏法脱硫的运行实践中,吸收塔溢流现象是许多火电厂经常出现的情况,浆液溢流不但易造成环境污染,还会对运行方式的控制产生不利的影响。为此结合天津国华盘山发电有限责任公司(简称国华盘电)FGD系统吸收塔浆液溢流的情况,分析其溢流原因及其控制措施。     

煤矸石和粉煤灰pH与电导率动态变化规律及其相关性研究

煤矸石和粉煤灰是煤矿区两种常见的固体废弃物,对环境造成极大的污染。pH波动幅度大是废弃物农用治理的主要障碍之一。对两种废弃物连续浸提时的pH和电导率(EC)进行长期动态监测,结果表明,不同层次的煤矸石尽管风化程度不同,但经过长时间浸取后,pH和EC变化趋势相似,且煤矸石、粉煤灰的pH、EC值有很大的相关性。该试验为今后两种废弃物合理利用奠定了基础。     

Editorial special issue on cyanobacterial blooms and water ecological restoration

Environmental Science and Pollution Research -     

Eddy current separation of broken lithium battery products in consideration of the shape factor

Journal of Material Cycles and Waste Management - Among the common recycling methods for lithium battery materials, pyrometallurgy recycling leads to high energy consumption and carbon emission...     

Effects of laser irradiation on a bloom forming cyanobacterium Microcystis aeruginosa

Environmental Science and Pollution Research - Effects of laser irradiation on photosystem II (PS II) photochemical efficiencies, growth, and other physiological responses of Microcystis aeruginosa...     

企业安全文化与HSE管理体系

从建立健康、安全与环境 (HSE)管理体系的基本思路、现状和发展趋势 ,以及中国石油化工集团公司HSE系列标准的内容、指导原则和建立HSE管理体系的理念等方面 ,阐述了HSE管理的建立、推行和发展的过程 ,HSE管理体系的建立和发展是石油石化企业在安全文化建设方面的重要成果。无论是安全管理的理念 ,或是生产经营活动都在不断创新和发展 ,都是培育和塑造中石化集团公司安全文化的具体体现。     

Spatial Dynamics of Soil Moisture in a Complex Terrain in the Semi‐Arid Loess Plateau Region,China1

Abstract: Soil moisture is an important hydrological variable in reforestation practices in a water‐limited region of the Loess Plateau of northwestern China. The objective of this study was to quantify the spatial dynamics of soil moisture on a complex terrain. During 2004‐2006, a total of 313 sample points in two kinds of grid (2 × 2 m and 20 × 20 m) were arranged for soil moisture measurements (two soil layers: 0‐30 and 30‐60 cm) with Time Domain Reflectometry. The geostatistical properties of soil moisture patterns, the variance and correlation structure of the soil moisture, and the effects of terrain factors on soil moisture were analyzed. The results suggested that our sampling grid captured the spatial variability of soil moisture distributions for this complex terrain. Principal Component Analysis and Cluster Analysis statistics showed that soil moisture decreased as slope gradient increased; that sunny aspects (112.5°‐292.5°) had relatively lower soil moisture than did shady aspects (292.5°‐112.5°); that soil moisture was lowest in the SWW direction and highest in the NWN direction; and that hillslope aspect was the main factor affecting soil moisture in the 0‐ to 30‐cm soil layer, whereas the main factor for the 30‐ to 60‐cm layer was slope gradient. It was found that the relative values of soil moisture for steep slopes (>36%) with shady aspect (292.5°‐112.5°), gentle slopes (<36%) with sunny aspect (112.5°‐292.5°), and steep slopes with sunny aspect were 99, 82, and 80, respectively – assuming a soil moisture value of 100 for gentle slopes with shady aspect. The results of this study are expected to be relevant to and useful for reforestation planning and design, parameterization of distributed hydrology models, and land productivity assessment in the study region.