EFFECTS OF FOREST FERTILIZATION ON STREAM WATER CHEMISTRY IN THE APPALACHIANS1

ABSTRACT: Stream water chemistry was monitored on two watersheds on the Fernow Experimental Forest in north-central West Virginia to determine the effects of forest fertilization on annual nutrient exports. Ammonium nitrate and triple superphosphate were applied simultaneously at rates of 336 kg ha^?1 N and 224 kg ha^?1 P₂O₅, respectively, which are similar to rates used in commercial forest operations. The treatment significantly increased outputs of several ions. Annual outputs of nitrate N increased as much as 18 times over pretreatment levels, and calcium and magnesium increased as much as three times over pretreatment levels the first year after fertilization. Outputs for these nutrients were elevated for all three post-treatment years. Although nitrate N increased significantly, only about 20 percent of the applied fertilizer was accounted for in stream water exports. Outputs of phosphate P declined following fertilization, probably because the watersheds are phosphorus deficient, but by the third year, they slightly exceeded predicted values. Estimated nutrient losses to deep seepage were substantial, especially on the leakier south-facing catchmeat, on which some nutrient losses were equal to or greater than those in stream water. When the nutrient exports associated with both stream discharge and ground water recharge were combined, the percentages of applied N that were lost were similar on the two watersheds, averaging 27.5 percent. Less than 1 percent of the applied P was lost from either watershed in the combination of streamflow and deep seepage.     

漂粉精生产过程中危险有害因素分析

通过对天津市漂粉精生产企业进行研究,分析了漂粉精生产过程可能存在的危险有害因素是尘毒、火灾、爆炸、灼伤、机械伤害等,并针对上述危险有害因素提出相应的防毒,防火防爆,防灼伤,防机械伤害等安全技术措施及安全管理措施.     

名山河流域黄壤无机纳米微粒对钙的吸附解吸特征

以名山河流域老冲积黄壤无机纳米微粒为对象,从纳米尺度分析钙的吸附解吸机制对土壤养分状况的影响,并采用等温吸附法和静态解吸法,比较不同土地利用方式下钙的吸附解吸特征差异.结果表明:1)不同土地利用方式土壤无机纳米微粒对钙的吸附解吸量均随钙质量浓度增加而增加,在低质量浓度范围内吸附量增加较快,在高质量浓度范围内增加趋缓,不同土地利用方式下钙的吸附能力从高到低为水田(2 580.69 mg/kg)、茶园(2 452.30 mg/kg)、旱地(1 935.10mg/ks)、林地(1 867.36mg/kg)、果园(1 520.65 mg/kg),土壤无机纳米微粒对钙的解吸率从大到小为果园、林地、旱地、茶园、水田,且解吸率随外加钙质量浓度增加而增大;2)去除土壤组分(有机质、游离氧化铁)后,无机纳米微粒对钙的吸附量及解吸量均有所增加,5种土地利用方式吸附增加量从大到小为水田、旱地、茶园、林地、果园;3)去除土壤组分前后,无机纳米微粒对钙的等温吸附均以Freundlich方程拟合效果最佳,相关系数在0.954 5～0.989 0,达到极显著水平,Langmuir方程与Temkin方程拟合效果不佳.研究表明,钙离子以非专性吸附为主,专性吸附为辅,有机质和游离氧化铁的存在会阻碍土壤对钙的吸附及解吸.     

秦淮河干流沉积物磷形态沿程分布特征

应用化学连续提取法,分析了秦淮河干流14个表层沉积物样品的磷形态沿程变化特征及其影响因素.结果发现,秦淮河干流由上游至南京市区段,随城市化程度的提高,河流沉积物总磷和各种形态磷沿程增加的趋势十分明显.Ca-P和Fe-P平均含量分别占TP的26.8%和25.7%,是主要的磷形态.易吸附态磷(L-P)在TP中的比例最低,但在城区由于TP的高度富集,其含量均超过15 mg·kg-1.沉积物中的总磷含量在城区河段显著增加,但只有很少部分转化为稳定形态的磷,人口密集区生活污水等各种来源排放的磷仍然深刻影响着城市河流的水环境质量.随城市化程度的提高,秦淮河中下游沉积物样品中钙富集的趋势明显,与之相对应的是沉积物Ca-P含量均超过200 mg·kg-1,相关分析和通径分析结果表明,二者之间存在成因上的联系.钙的富集提高了沉积物的固磷能力,将上覆水体中的磷转化为钙结合态磷.城区河流沉积物中钙含量的升高,对于河流生态系统磷的迁移转化有重要影响.     

Se-Ca联合膳食干预缓解Cd诱导小鼠肝肾毒性

为探究Se-Ca联合膳食干预对生物Cd中毒的缓解效果,选取88只BALB/c小鼠,随机划分为19组,在相同饲料Cd暴露浓度下(2mg/kg)分别设置低、中、高浓度的Se和Ca单独和联合膳食干预处理,并观察30d后小鼠的生长发育、肝肾功能、氧化应激状态和组织病理变化.结果显示,Se-Ca联合干预可有效缓解Cd蓄积所致小鼠生长发育迟缓现象,且进一步促进小鼠生长;肝肾功能及氧化应激指标测定结果表明,Se-Ca联合干预对Cd暴露下小鼠肝脏AST、GSH、SOD、GSH-Px和肾脏BUN、MDA、SOD的保护效果优于单一元素干预;联合干预仅需较小剂量即可达到单独Se或Ca干预对肝肾病理损伤的最佳缓解效果.Se-Ca联合膳食干预可有效缓解Cd摄入导致的生长发育缓慢和肝肾毒性,且较之单一元素的干预效果更佳.     

铁基硅盐对土壤环境镉砷赋存形态及转化影响

为探明铁基硅盐对土壤镉砷赋存形态影响及各形态间转化规律,采用室内长期淹水培养吸附实验,研究不同比例铁硅材料对土壤离子态镉砷活性影响;筛选适宜铁基硅盐(FS)配比同时添加腐殖酸(FSC)和金属氧化物(FSCa),明确复配处理土壤中镉砷分级形态转化程度.结果显示,铁:硅比值增加10%,土壤pH值平均降低0.35;F₂-S₈处理土壤离子态镉降幅71%;F₁₀-S₀处理土壤离子态砷降低59.9%,离子态镉砷含量与硅酸盐-铁盐施用量互呈反比;处理F₄-S₆和F₆-S₄之间镉、砷钝化率产生交点,约为25%~30%.土壤中镉主要以可溶态为主,占比58%;砷主要以铁铝氧化态和钙结合态为主,占比40%和23%.铁硅比例为5:5或5.5:4.5左右复配能有效将铝结合态砷和铁铝氧化态砷转变为钙结合态砷和残渣态砷,可溶态镉转化为碳酸盐结合态镉以及铁锰氧化态镉,同步降低土壤中镉砷的活性.     

The variability and intrinsic remediation of a BTEX plume in anaerobic sulphate-rich groundwater

Data from long-term groundwater sampling, limited coring, and associated studies are synthesised to assess the variability and intrinsic remediation/natural attenuation of a dissolved hydrocarbon plume in sulphate-rich anaerobic groundwater. Fine vertical scale (0.25- and 0.5-m depth intervals) and horizontal plume-scale (>400 m) characteristics of the plume were mapped over a 5-year period from 1991 to 1996. The plume of dissolved BTEX (benzene, toluene, ethylbenzene, xylene) and other organic compounds originated from leakage of gasoline from a subsurface fuel storage tank. The plume was up to 420 m long, less than 50 m wide and 3 m thick. In the first few years of monitoring, BTEX concentrations near the point of leakage were in approximate equilibrium with non-aqueous phase liquid (NAPL) gasoline. NAPL composition of core material and long-term trends in ratios of BTEX concentrations in groundwater indicated significant depletion (water washing, volatilisation and possibly biodegradation) of benzene from residual NAPL after 1992. Large fluctuations in BTEX concentrations in individual boreholes were shown to be largely attributable to seasonal groundwater flow variations. A combination of temporal and spatial groundwater quality data was required to adequately assess the stationarity of plumes, so as to allow inference of intrinsic remediation. Contoured concentration data for the period 1991 to 1996 indicated that plumes of toluene and o-xylene were, at best, only partially steady state (pseudo-steady state) due to seasonal groundwater flow changes. From this analysis, it was inferred that significant remediation by natural biodegradation was occurring for BTEX component plumes such as toluene and o-xylene, but provided no conclusive evidence of benzene biodegradation. Issues associated with field quantification of intrinsic remediation from groundwater sampling are highlighted. Preferential intrinsic biodegradation of selected organic compounds within the BTEX plume was shown to be occurring, in parallel with sulphate reduction and bicarbonate production. Ratios of average hydrocarbon concentrations to benzene for the period 1991 to 1992 were used to estimate degradation rates (half-lives) at various distances along the plume. The estimates varied with distance, the narrowest range being, for toluene, 110 to 260 days. These estimates were comparable to rates determined previously from an in situ tracer test and from plume-scale modelling.     

氯化钙种子气溶胶对甲苯二次有机气溶胶与氨形成含氮有机物的影响

苯系物光氧化反应形成的二次有机气溶胶(SOA)是大气细粒子的重要组成部分.SOA羧酸和二元醛组分能与氨反应形成有机酸铵和咪唑类含氮有机物,它们能够吸收205 nm和270 nm的紫外辐射,是棕色碳的主要组分.氯化钙等无机种子气溶胶具有较大的比表面积,可为气相羰基化合物和氨提供凝结与反应载体,从而影响含氮有机物的形成.基于此,本文利用烟雾腔研究氯化钙种子气溶胶存在时甲苯SOA与氨的反应,采用紫外-可见分光光度计测量产物溶液在205 nm和270 nm处的吸光度,并定性研究不同浓度、湿度和酸度的氯化钙种子气溶胶对含氮有机物形成的影响.结果表明:氯化钙种子气溶胶能够促进甲苯SOA含氮有机物的形成;含氮有机物的生成浓度随着氯化钙种子气溶胶浓度和pH值的增加而逐渐增大.但当氯化钙种子气溶胶为碱性时,OH~-会与凝结的有机酸发生酸碱中和反应并抑制二元醛化合物水合形成四醇产物,从而不利于含氮有机物的生成;水分子的增加占据了氯化钙种子气溶胶表面的吸附活性位点,氨被吸附和凝结的量减少,从而导致含氮有机物的生成浓度随着相对湿度的增大而降低.本研究可为人为源SOA棕色碳的形成机制和化学组成研究提供实验依据.     

Fe(VI)/CaO2双氧化体系降解水环境中的DMP

研究了高铁酸盐（Fe（VI））/过氧化钙（CaO₂）联合处理对邻苯二甲酸二甲酯（DMP）的降解性能及机理,分析了共存离子的影响.基于响应面方法中的Box-Behnken实验设计进行了多因素实验,采用二次多项式和逐步回归法拟合了DMP去除率与Fe（VI）投加量、CaO₂投加量和反应时间之间的关系,对实验条件进行了优化分析.结果表明,在初始pH值为中性条件下,Fe（VI）/CaO₂可以有效去除DMP,降解过程符合准一级动力学模型.当Fe（VI）/CaO₂/DMP物质的量比为1.1/4.4/1时,模型预测DMP最大降解率为95.57%,和验证实验得出的降解率90.14%相近,表明该响应面模型具有较好的模拟和预测能力.HCO₃^-和Mg²⁺对DMP的降解有一定抑制作用.自由基清除实验结果显示,羟基自由基（HO·）和超氧自由基（O₂^-·）对DMP的降解具有重要贡献,表明Fe（VI）和CaO₂可形成类芬顿试剂协同降解污染物.DMP的主要降解途径包括酯基水解、侧链氧化和苯环的羟基化;主要降解产物为邻苯二甲酸单甲酯,2,5-二羟基苯甲酸,间苯二甲酸,草酸等.     

煤燃烧过程中有机钙固氟效果研究

选择醋酸钙镁、醋酸钙2种有机钙为固氟剂,在固定床管式炉上对它们的固氟效果进行了初步研究,并分析了粒径、温度、钙硫比等对试验结果的影响.通过与传统固氟剂碳酸钙的固氟效果进行比较发现:在相同实验条件下,这2种有机钙具有良好的固氟效果,高温阶段效果更加明显,温度为1 000～1 100℃时,醋酸钙镁的固氟率是碳酸钙的1.68～1.74倍,醋酸钙的固氟率为碳酸钙的1.28～1.37倍.