基于高分影像的城市黑臭水体遥感识别:以南京为例

城市黑臭水体的遥感识别对于黑臭水体的监测、治理有着重要作用.2016年对南京城市河段进行了地面调查,并在沙洲西河、秃尾河、玄武湖、金川河设置了55个样点,采集水样分析水质参数并同步测量水面光谱.在此基础上,利用绿光波段遥感反射率的单波段阈值、蓝、绿波段差值、红、绿波段比值,以及色度值,分别构建了基于GF-2影像的城市黑臭水体遥感识别算法,并分析南京市主城区黑臭水体的空间分布和环境特点.结果表明:(1)和其他类型水体相比,城市黑臭水体遥感反射率最低,在整个可见光范围峰谷不突出,而且在400~550 nm范围光谱斜率最小;(2)采用地面同步调查结果检验,比值算法的识别精度最高,对城市河道黑臭水体的识别更准确;(3)利用比值法对2016年11月3日的GF-2影像进行计算,共提取研究区黑臭河段11条,总长度40.7 km,总面积0.749 km~2.黑臭河段分布具有范围广且不连续的特征,集中分布于各城区人口密集的区域;水体发生黑臭主要受到生活污水、工业废水、断头浜的影响.     

小波分析在湖泊常见浮游藻荧光识别测定中的应用

利用Daubechies7（db7）小波函数对27种分属于6个门,22个属的主要湖泊常见浮游藻的三维荧光光谱进行分解,得到各尺度分量及小波分量,应用Bayesian判别分析选择第三层尺度分量（Ca3）作为最佳特征谱,通过系统聚类分析得到浮游藻的标准谱库,结合非负最小二乘法解析的多元线性回归建立湖泊常见浮游藻的荧光识别测定技术.将该技术用于单种藻样品、模拟混合样品及实际混合样品的识别分析,单种藻样品在门类水平上的识别正确率平均为98.6%,识别测定的平均相对含量为90.8%.在实验过程中加入一定比例的噪声,考察了标准谱库的抗噪能力.对于104个实验室混合样品,优势门的藻在门类水平上的平均识别正确率为97.0%,识别的平均相对含量为67.7%,次优势门的藻在门类水平上的平均识别正确率为90.7%,识别的平均相对含量为32.3%.结果表明,所建立的识别测定技术具有可行性.     

太阳辐射试验标准中的太阳光谱分布

目的为太阳辐射试验标准、光老化试验标准修订时正确选择太阳光谱提供依据。方法辨析CIE NO.20,CIE NO.85两种出版物太阳辐射光谱特点,从五个方面对此问题进行探讨,统计这两种太阳辐射光谱带宽辐照度的误差;分析相对空气质量、臭氧与水分、云层光学厚度、地表反射率等因素对太阳辐射光谱辐照度的影响;分析人工辐射光源光谱分布特点,以及它们与太阳辐射光谱的差别;分析当前光老化试验标准对光谱辐照度允差的要求;介绍光老化试验结果间的可比性。结果 CIE NO.85光谱更准确、更细致,但其波长范围较窄,两种光谱辐照度的差别很小,大气环境中许多因素会降低到达地面的光谱辐照度;人工辐射光源光谱与太阳光谱的误差、光老化试验标准中光谱辐照度允差都远大于前述太阳辐射光谱间的误差,标准对太阳光谱波长范围的要求比CIE NO.85光谱宽。结论太阳辐射试验标准、光老化试验标准修订时,仍可选用CIE NO.20光谱作为太阳辐射光谱。     

Adsorption of Ca2+ on single layer graphene oxide

Graphene oxide(GO) holds great promise for a broad array of applications in many fields,but also poses serious potential risks to human health and the environment.In this study,the adsorptive properties of GO toward Ca~(2+) and Na+were investigated using batch adsorption experiments,zeta potential measurements,and spectroscopic analysis.When pH increased from 4 to 9,Ca~(2+)adsorption by GO and the zeta potential of GO increased significantly.Raman spectra suggest that Ca~(2+)was strongly adsorbed on the GO via –COO Ca~+ formation.On the other hand,Na+was adsorbed into the electrical diffuse layer as an inert counterion to increase the diffuse layer zeta potential.While the GO suspension became unstable with increasing pH from 4 to 10 in the presence of Ca~(2+),it was more stable at higher pH in the NaC l solution.The findings of this research provide insights in the adsorption of Ca~(2+)on GO and fundamental basis for prediction of its effect on the colloidal stability of GO in the environment.     

不同原料生物质炭DOM组分成分特性

不同原料的生物质炭DOM含量和组分存在差异,选取水稻秸秆（RS）、小麦秸秆（WS）、大豆秸秆（SS）、油菜秸秆（YS）、花生壳（PH）、松木屑（PW）和竹粉（BS）7种生物质原料在450 ℃下制备的生物质炭,采用紫外-可见光光谱（UV-vis）、荧光光谱（EEM）结合平行因子分析（PARAFAC）技术对生物质炭中DOM的光谱特征和荧光组分进行表征.结果表明：木本类生物质炭的DOM含量较秸秆类生物质炭低,分子量较高.从生物质炭DOM中鉴定分离可见区类富里酸组分（C1）、较短波长类腐殖酸组分（C2）、较长波长类腐殖酸组分（C3）和类蛋白质组分（C4）等4种组分.不同原料生物质炭DOM各组分的最大荧光强度（F_max）值表现为C1 ＞ C2 ＞ C3 、C4,秸秆类炭DOM各组分的F_max值显著高于木本类.生物质炭DOM中以C1组分占主导地位,占比达48.87% ~ 79.97%.C2、C3组分在YSB、SSB-DOM中占比最高,分别达32.71%和23.25% ,仅在YSB和PHB-DOM中发现少量C4组分.木本类原料的有机和无机矿物含量远低于秸秆类,原料中纤维素含量与生物质炭DOM总量及其C3组分呈显著的正相关关系, Ca含量与生物质炭的DOM含量及其F_max值和C3组分呈显著正相关,说明不同生物质原料的组成对生物质炭DOM组成特性具有显著的影响,研究结果为全面评估不同原料生物质炭DOM的环境效应提供重要的科学理论依据.     

三峡库区消落带土壤中溶解性有机质(DOM)吸收及荧光光谱特征

利用紫外-可见吸收光谱和三维荧光光谱技术,结合荧光区域积分法,分析了三峡库区消落带土壤DOM的地化特征.结果表明,各区县消落带土壤CDOM平均浓度大小顺序为:忠县丰都涪陵万州巫山云阳奉节开县,其中,忠县、丰都和涪陵土壤CDOM浓度[a(355)]、芳香性(SUVA254)和疏水组分(SUVA260)明显高于其它区县,而其腐殖化程度(HIX)均低于其它区县.三峡库区消落带土壤DOM中含有类腐殖质荧光团A、C、M和类色氨酸荧光团T,其中紫外区类腐殖质荧光团A的荧光区域积分比例最大.另外,类色氨酸荧光团T与a(355)呈极显著相关(r=0.674,P0.01),影响CDOM浓度变化的主要因素是类蛋白荧光峰T.3D-EEM总荧光强度(TOT)可作为表征三峡库区消落带土壤CDOM荧光团浓度的指标.消落带土壤DOM腐殖化程度较低,生物可利用性较高.另外,消落带干湿交替作用对不同高程土壤DOM地化特征影响的差异较小,这可能与当地农业活动、沿岸植物生长以及DOM矿化过程有关.     

微生物燃料电池降解焦化废水过程研究

焦化废水生化处理流程复杂，污染物降解过程尚不明确，构建无膜空气阴极焦化废水微生物燃料电池，利用循环伏安法、红外分析、微生物群落结构等分析考察了焦化废水的降解过程中，各类有机物含量变化、官能团的变化、有机物异步降解次序及优势菌种的演替.焦化废水中含硫无机物被优先降解，酚类降解次之，含氮污染物历经好氧硝化与厌氧反硝化降解过程，但落后于前者；长链烷烃类降解缓慢；生物群落结构与底物中有机物种类密切相关，初期Desulfurella优先氧化含硫污染物、Flavobacterium降解酚类次之、Nitrospirae氧化降解NH₄⁺-N较为缓慢，随时间延长Alcaligenes、Thiobacillus演变为优势菌落，实现了酚类的降解及NO₃^-的反硝化降解；电池输出电压为470.9mV，最高输出功率密度达12.5mW/cm²，COD、T_phenols、T_surful、TN、NH₄⁺-N的降解分别为85.8%、83.3%、87.5%、43.8%、89.9%.利用微生物燃料电池技术处理焦化废水，一步实现水质净化及能量回收，为废水生物处理控制提供理论和实践参考.     

Moist Olive Husks Addition to a Silty Clay Soil: Influence on Microbial and Biochemical Parameters

To investigate the effects of moist olive husks (MOH-residues) on soil respiration, microbial biomass, and enzymatic (o-diphenoloxidase, β-glucosidase, dehydrogenase and alkaline phosphatase) activities, a silty clay soil was incubated with 0 (control), 8 × 10³ (D), 16 × 10³ (2D) and 80 × 10³ (10D) kg ha^?1 of MOH-residues on a dry weight basis. Soil respiration and microbial biomass data indicated that the addition of MOH-residues strongly increased microbial activity proportionally to the amounts added. Data of qCO₂ suggested that the respiration to biomass ratio of the microbial population was strongly modified by MOH-residues additions during the first 90 days of incubation. The qCO₂ data suggested a low efficiency in energy yields from C oxidation during the first 2 months of soil incubation. qFDA seemed to be relatively unaffected for treatments D and 2D as compared to the control, but was significantly lowered by the application of 10D, showing the lowest hydrolytic activity of microbial biomass in this treatment up to 360 days of incubation.

o-Diphenoloxidase activity was delayed, and this delay was extended with the addition of larger quantities of MOH-residues. Alkaline phosphatase, β-glucosidase and dehydrogenase activities were in line with the findings on microbial biomass changes and activities. The biological and biochemical data suggest that the addition of a large quantity of MOH-residues (80 × 10³ kg ha^?1) strongly modifies the soil characteristics affecting the r- and K-strategist populations, and that these changes last for at least the 360 days of incubation. The data also suggest that application rates exceeding 16 × 10³ kg ha^?1 are not recommended until the agro-chemical and -physical functions of the soil are further studied.     

Effect of sunlight radiation,rainfall and droplet spectra of sprays on persistence of bacillus thuringiensis deposits after application of dipel® 76af formulation onto conifers

Abstract

The effect of sunlight radiation, rainfall and droplet spectra of sprays on per ‐sistence of a Bacillus thuringiensis subspp. kurstaki (Btk) formulation, DiPel^® 76AF, was examined after application onto spruce [Picea glauca (Moench) Voss] foliage. The investigation consisted of three studies: (i) Study I: a laboratory microcosm study to examine the photostability of DiPel 76AF deposits on foliage after different periods of exposure to two radiation intensities, (ii) Study II: a laboratory microcosm study to examine the rainfastness of foliar deposits after exposure to different amounts of rainfall consisting of two separate droplet spectra, and (iii) Study III: a field microcosm study to investigate the influence of two different droplet spectra of DiPel 76AF sprays on foliar persistence of Btk under natural weathering conditions. In all studies, persistence of Btk was investigated both by bioassay [using spruce budworm (Choristoneura fumiferana Clemens)] and total protein assay.

The findings of Study I indicated that bioactivity of foliar deposits decreased with increasing duration of exposure to radiation, and with increasing radiation intensity. The half‐life (DT₅₀, the exposure period required for 50% of the initial bioactivity to disappear) was 5.1 d for the low intensity, and 3.9 d for the higher intensity. In contrast with the bioassay results, the total protein levels [determined by the bicinchoninic acid (BCA) method] showed no decrease with increasing duration of exposure, or with increasing radiation intensity.

The findings of Study II indicated that bioactivity of foliar deposits decreased with increasing cumulative rainfall. A new term, RF₅₀ [the amount of rain (in mm) required to washoff 50% of the initial deposit], was introduced to understand the relationship between rainfall intensity and reduction in bioactivity. When the same amount of rain was applied in different droplet sizes, the RF₅₀ value was high (5.2 mm) for the small rain droplets, and was low (2.9 mm) for the large rain droplets. Similar to the bioassay results, the total protein concentrations (determined by the BCA method) decreased with increasing amount of rain and with increasing rainfall intensity. The RF₅₀ value (obtained using ng protein /cm²) was 5.4 mm for the small rain droplets, and was 3.4 mm for the large rain droplets.

The field microcosm study indicated that when DiPel 76AF was applied in small droplets (D_v.5 of 65 μm), the persistence of bioactivity was ca 8.0 d, whereas when it was applied in large droplets (D_v.5 of 130 nm) it was ca 11 d. Bioactivity decreased with time after spray, and the DT₅₀ was 1.98 d for the spray of small droplets, and 2.87 d for that of large droplets. Similar to the bioactivity, the total protein concentrations also decreased with time after spray, and the DT₅₀ values for the small and large droplet spectra were 3.45 and 6.07 d respectively.     

月球紫外-可见-近红外反射光谱的基本特征及解析方法

月球紫外-可见-近红外反射光谱(强度,反照率以及吸收特征)是研究月球表面物质组成的重要手段。文章简要介绍了月球表面反射光谱的基本特征、形成机制以及现有月球反射光谱数据及其解析方法。这些方法主要有光谱参数、连续背景扣除、高斯反卷积分析以及主成分分析。还讨论了高光谱探测器在月球探测中的应用前景、已有方案以及获取新的月球样品对月球反射光谱研究的重要性。