川中丘陵区村级景观土壤有机碳密度和储量分析

本文综合运用了地理信息系统(GIS)、遥感(RS)和全球卫星定位系统(GPS)等技术手段,分析了人口密集的川中丘陵乡村区域土壤有机碳密度(SOCD)和储量(SOCS)的空间分布及影响因素。结果表明,区域内SOCD和SOCS平均值分别为5.58kg/m2和75.77×105g,SOCD随丘体高度的降低向四周逐渐增大,SOCS主要分布于旱地、水田等土地利用类型中。0~30cm土层和土体深度内,SOCD以冬水田最高,裸岩最低;SOCS则以丘脚旱地和轮作水田最高,裸岩最低。地形、土地利用和土地覆盖对SOCD、SOCS影响明显。     

活性炭纤维复合材料的脱硫性能

本实验以粘胶基活性炭纤维和酚醛树脂复合,制备出了一种可用于烟气脱硫的活性炭纤维复合材料（ACFM）,考察了制备工艺条件对脱硫性能和比表面积的影响,测试其在填充床的压降。结果表明：粘结剂用量、炭化及活化条件对样品的脱硫性能和比表面积有较大的影响;与其他活性炭材料相比ACFM压降相对较低,只有活性炭纤维的1／20。     

Predicting Water Quality Impaired Stream Segments using Landscape-Scale Data and a Regional Geostatistical Model: A Case Study in Maryland

In the United States, probability-based water quality surveys are typically used to meet the requirements of Section 305(b) of the Clean Water Act. The survey design allows an inference to be generated concerning regional stream condition, but it cannot be used to identify water quality impaired stream segments. Therefore, a rapid and cost-efficient method is needed to locate potentially impaired stream segments throughout large areas. We fit a set of geostatistical models to 312 samples of dissolved organic carbon (DOC) collected in 1996 for the Maryland Biological Stream Survey using coarse-scale watershed characteristics. The models were developed using two distance measures, straight-line distance (SLD) and weighted asymmetric hydrologic distance (WAHD). We used the Corrected Spatial Akaike Information Criterion and the mean square prediction error to compare models. The SLD models predicted more variability in DOC than models based on WAHD for every autocovariance model except the spherical model. The SLD model based on the Mariah autocovariance model showed the best fit (r² = 0.72). DOC demonstrated a positive relationship with the watershed attributes percent water, percent wetlands, and mean minimum temperature, but was negatively correlated to percent felsic rock type. We used universal kriging to generate predictions and prediction variances for 3083 stream segments throughout Maryland. The model predicted that 90.2% of stream kilometers had DOC values less than 5 mg/l, 6.7% were between 5 and 8 mg/l, and 3.1% of streams produced values greater than 8 mg/l. The geostatistical model generated more accurate DOC predictions than previous models, but did not fit the data equally well throughout the state. Consequently, it may be necessary to develop more than one geostatistical model to predict stream DOC throughout Maryland. Our methodology is an improvement over previous methods because additional field sampling is not necessary, inferences about regional stream condition can be made, and it can be used to locate potentially impaired stream segments. Further, the model results can be displayed visually, which allows results to be presented to a wide variety of audiences easily.     

生物活性炭法深度处理印染废水及其生物毒性的表征

采用负载经驯化后微生物的活性炭深度处理实际印染废水,研究生物活性炭系统中存在的生物相及其降解有机污染物的作用,并表征了处理后印染废水的生物毒性.结果表明,生物相中含有草履虫、轮虫及钟虫等原生动物.随着运行次数的增加,活性炭反应器在运行5次后出水的COD、NH3-N及色度去除率骤降,但是生物活性炭处理后出水的COD、NH3-N及色度去除率缓慢下降.生物活性炭能很好地降解印染废水中的苯酚类和稠环芳烃污染物.本研究中生物活性炭反应器对氨氮和COD的去除符合一级动力学方程,去除动力学常数分别为1.02和0.96.经过生物活性炭的处理可以将印染废水的生物毒性降到适于小球藻生长的水平.     

超声前处理强化活性炭吸附活性艳红X-3B染料废水

探究了超声前处理活性艳红X-3B染料废水强化活性炭吸附降解性能及不同超声参数的影响规律,包括超声功率和超声时间。研究结果表明,超声前处理活性艳红X-3B染料废水可通过空化效应使有机大分子裂解为小分子易于被活性炭吸附,同时可强化其到活性炭微孔中传输,提高了活性炭吸附降解性能,最佳超声功率为320 W。浓度越高,所需超声时间越长,当超声达到一定时间后,继续超声不会影响染料分子的吸附。超声前处理虽然不会改变吸附平衡时间,但可有效增加活性炭处理活性艳红X-3B染料废水的饱和吸附量。     

大气颗粒物中元素碳的直接测定

对原来用元素分析仪测定大气颗粒物样品中有机碳、元素碳的方法[1 ] 进行改进 ,将差减法间接测定元素碳改为一步直接测定元素碳。有机碳、元素碳的测量标准偏差的平均值分别为 0 35 %、0 34% ,提高了元素碳的测量精度 ,同时避免了误差传递 ,解决了差减法测定元素碳时出现负值的情况。     

Effects of chemical modification on physicochemical properties and adsorption behavior of sludge-based activated carbon

This study aimed to explore the adsorption performance of sludge-based activated carbon (SBC) towards dissolved organic matters (DOMs) removal from sewage, and investigated the modification effect of different types of chemicals on the structure of synthesized SBC. Waste activated sludge (WAS) was used as a carbon source, and HCl, HNO₃, and NaOH were used as different types of chemicals to modify the SBC. With the aid of chemical activation, the modified SBC showed higher adsorption performances on DOMs removal with maximum adsorption of 29.05 mg/g and second-order constant (k) of 0.1367 (L/mol/sec) due to the surface elution of ash and minerals by chemicals. The surface elemental composition of MSBC suggested that the content of C-C and C-O functional groups on the surface of modified sludge-based activated carbon (MSBC) played an important role on the adsorption capacities of MSBC towards DOMs removal in sewage. Additionally, the residual molecular weight of DOMs in sewage was investigated using a 3-dimension fluorescence excitation-emission matrix (3D-EEM) and high-performance size exclusion chromatography (HP-SEC). Results showed that the chemical modification significantly improved the adsorption capacity of MSBC on humic acids (HA) and aromatic proteins (APN), and both of NaOH-MSBC and HCl-MSBC were effective for a wide range of different AMW DOMs removal from sewage, while the HNO₃-MSBC exhibited poorly on AMW organics of 2,617 Da and 409 Da due to the reducing content of macropore. In brief, this study provides reference values for the impact of the chemicals of the activation stage before the SBCs application.     

活性炭纤维处理甲苯废气试验研究

采用动态吸附试验,研究了进气温度、废气浓度对粘胶基活性炭纤维吸附甲苯过程的影响,分析了活性炭纤维(ACF)的穿透时间、平衡饱和吸附量的变化情况,并用Y-N模型对穿透曲线进行拟合.研究了吸附饱和ACF采用氮气热再生法,确定了温度、流量、再生时间等最佳操作参数,并进行了相关机理的探讨.     

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。     

湘东丘陵区不同类型土壤活性碳组分的剖面分布与差异

土壤活性碳组分是土壤健康变化的指示器。选取湘东丘陵区3种不同母质发育的林地土壤（紫色土、板岩红壤和花岗岩红壤）,研究土壤颗粒有机碳（POC）和溶解性有机碳（DOC）的剖面分布规律,并分析POC、DOC与土壤有机碳（SOC）、土壤质地的关系。结果表明：土壤剖面POC、DOC质量分数分别介于0．29～3．87g·kg。和15．01～311．34mg·kg^-1,随剖面加深而大幅降低。土壤剖面POC储量介于8．61一16．54t·hm^-2,以花岗岩红壤最高,板岩红壤最低;而DOC储量介于380．76～1184．83kg·hm^-2,以板岩红壤最高,紫色土最低。POC占SOC的比例（POC／SOC）介于6．42％～46．25％,其中紫色土和板岩红壤POC／SOC随土层加深而降低,而花岗岩红壤则完全相反。DOC占SOC的比例（DOC／SOC）介于O．35％～3．02％,其中紫色土DOC／SOC随土层加深而降低,板岩红壤与花岗岩红壤DOC／SOC则以B层最高。由此可见,不同母质发育的土壤类型,碳库质量和脆弱程度不一。从维持地力和环境健康的角度,应对不同母质发育的土壤制定不同的开发利用方案。