固定源细颗粒物稀释测试法现场应用存在问题及影响因素分析研究

对基于大气环境的稀释测试法在现场应用中存在的主要问题进行了归纳总结,并对若干影响细颗粒物测试结果的重要因素进行了分析,诸如停留时间、稀释比、采样时间等因素,期望能够对该法测试系统的后续改进或重新设计提供实际问题导向,同时也能够对该领域现场工作的科研人员提供非常有用的经验。     

牡蛎壳粉和石灰改良酸性水稻土对磷有效性、形态和酶活性的影响

我国南方粮食主产区土壤酸化治理是提升耕地地力促进粮食增产的重要内容,目的是探究酸化土壤改良剂牡蛎壳粉和石灰对水稻土酸度、磷有效性和形态以及酶活性和相关功能基因的影响.盆栽试验设计2种改良剂的3个施用量（0.05%、0.10%和0.15%）,以水稻为试验作物.结果表明：①牡蛎壳粉和石灰均显著提高土壤pH,降低土壤交换性酸,且改良效果随着改良剂用量增加而提高,相同用量下石灰对土壤酸性的改良效果高于牡蛎壳粉;② 4种有效磷提取剂提取的土壤有效磷测定结果表明,牡蛎壳粉和石灰显著提高H₂SO₄-P、Bray-1 P和Olsen-P含量,其中Olsen-P含量随改良剂用量的增加而提高.③土壤中不同形态无机磷含量表现为：Fe-P>Al-P>Ca-P,石灰和牡蛎壳粉显著提高Al-P和Fe-P含量,分别提高26.3%~37.4%和7.9%~23.7%;0.15%改良剂显著增加Ca-P含量;④石灰和牡蛎壳粉对土壤DHA、ALP、IPP活性和phoD基因拷贝数具有提高作用,而对土壤ACP活性、phoC和pqqC拷贝数表现为降低;⑤改良剂（0.10%和0.15%）显著提高水稻产量,0.15%用量的石灰和牡蛎壳粉分别提高水稻产量34.2%和46.8%,但对秸秆生物量无显著影响.相关分析表明,土壤无机磷和有效磷含量与pH和ALP活性呈显著正相关,改良剂通过消除土壤酸化和提高土壤磷酸酶活性来改善土壤磷营养状况,这对促进作物产量具有积极作用.     

大气气溶胶酸度和酸化缓冲能力研究

为了掌握大气气溶胶与酸性降水的关系 ,分析和研究了中国北方和南方不同观测点可吸入颗粒物 (PM10 )的酸度 ,并利用微量酸碱滴定的方法测定了其酸化缓冲能力。结果表明大气气溶胶具有一定的酸度 ,同时对酸化的缓冲能力非常低 ,甚至可以促进降水的酸化 ,这种污染特征也是上述观测点发生酸性降水的重要原因之一。     

Titration Curves: A Useful Instrument for Assessing the Buffer Systems of Acidic Mining Waters (10 pp)

Background, Aims and Scope The acidification of mine waters is generally caused by metal sulfide oxidation, related to mining activities. These waters are characterized by low pH and high acidity due to strong buffering systems. The standard acidity parameter, the Base Neutralization Capacity (BNC) is determined by endpoint titration, and reflects a cumulative parameter of both hydrogen ions and all buffering systems, but does not give information on the individual buffer systems. We demonstrate that a detailed interpretation of titration curves can provide information about the strength of the buffering systems. The buffering systems are of importance for environmental studies and treatment of acidic mining waters. Methods Titrations were carried out by means of an automatic titrator using acidic mining waters from Germany and Canada. The curves were interpreted, compared with each other, to endpoint titration results and to elemental concentrations contained therein. Results and Discussion The titration curves were highly reproducible, and contained information about the strength of the buffer systems present. Interpretations are given, and the classification and comparison of acidic mining waters, by the nature and strength of their buffering systems derived from titration curves are discussed. The BNC-values calculated from the curves were more precise than the ones determined by the standard endpoint titration method. Due to the complex buffer mechanisms in acidic mining waters, the calculation of major metal concentrations from the shape of the titration curve resulted in estimates, which should not be confused with precise elemental analysis results. Conclusion Titration curves provide an inexpensive, valuable and versatile tool, by which to obtain sophisticated information of the acidity in acidic water. The information about the strength of the present buffer systems can help to understand and document the complex nature of acidic mining water buffer systems. Finally, the interpretation of titration curves could help to improve treatment measurements and the ecological understanding of these acidic waters.     

动态稀释校准仪对VOCs自动监测系统的影响

基于环境空气VOCs自动监测系统中动态稀释校准仪在相同稀释比和不同稀释流量条件下,对仪器测试结果误差的影响进行研究,指出了当前环境空气VOCs自动监测普遍使用的校准仪的不足之处。选取臭氧前体物(PAMS) 57种有机化合物,以不同稀释总流量,分别测试0. 5和1. 0 nmol/mol的平均检出限以及平均回测偏差,结果显示,在输出流量1 000 m L/min时,平均检出限分别在0. 02～0. 17和0. 01～0. 10 nmol/mol;平均回测偏差在-12%～26%和-28%～10%。当总输出流量 1 000 m L/min时,多点曲线各浓度点重复性5%。     

鼎湖山针阔叶混交林土壤酸度与土壤养分的季节动态

研究了鼎湖山南亚热带森林演替系列中处于中间阶段的针阔叶混交林土壤的pH值、水解氮、速效磷、钾、交换性钙、镁等几种营养元素的含量现状及季节动态。结果表明：混交林土壤为强酸性土壤，表层(0--20cm)土壤酸度高于中(20--40cm)、下(40-60cm)层土壤，0～40cm土壤pH值具有明显的季节波动性。降雨、温度、凋落物、植物根系以及微生物的活动等因素可能是鼎湖山混交林土壤pH值季节动态变化的主要因素。除Ca外，在同一剖面内，表层土壤养分的含量明显高于中下层，而中下层之间相差不大，养分大多在冬季较高，随着季节变动(1，4，7，10月)呈下降趋势。     

Effects of golden shiner (Notemigonuscrysoleucas ) nest association on host pumpkinseeds (Lepomisgibbosus ): evidence for a non-parasitic relationship

The reproductive success of male parental pumpkinseeds, Lepomisgibbosus, was studied in relation to the use of their nests by spawning golden shiners, Notemigonuscrysoleucas. The brood size of pumpkinseeds with and without golden shiner's young was compared in a field population. Mean egg and larval numbers of pumpkinseeds did not differ between broods with and without shiners, suggesting that shiners had no net effect on the fitness of host pumpkinseeds. In the laboratory, however, hatching success of pumpkinseed embryos was significantly lower with shiners than without. This difference was attributable to fungal infection. Against this fitness loss, the presence of shiner larvae reduced predation on pumpkinseed larvae in laboratory experiments. Thus, two counteracting mechanisms are proposed to account for no observed net effect on the host: (1) increased fungal infection on pumpkinseed embryos and (2) decreased predation on pumpkinseed young. Received: 10 January 1997 / Accepted after revision: 9 August 1997     

Geochemical Characteristics of the Acid Mine Drainage in the Water System in the Vicinity of the Dogye Coal Mine in Korea

This study investigated geochemical characteristics of the acid mine drainage (AMD) discharged from the abandoned mine adits in the vicinity of the Dogye coal mine in Korea. Acid mine drainage discharged from Jeoncha pit adit of the Dogye coal mine, which is the main source of the AMD in the study area, had a pH value of 3.0 and concentrations of 2148mg SO₄ ^2– L^–1, 229mg Fe L^–1, 71mg A1 L^–1 and 11mg Mn L^–1. The reduction of some metal concentrations downstream from the discharge point could be explained on the basis of dilution and precipitation. The order of removal of metal ions downstream from the discharge point was Fe>A1, Cu>Zn, Mn. Acidity could be used as a good determining factor offering comprehensive and quantitative values for the polluting extent of acid mine drainage. The acidities existing in all acidic water samples in the Gunahan district originated primarily from mineral acidity, especially in the upper Nahan Creek from dissolved Fe and Al and in the middle and down Nahan Creek from dissolved Al. From the application of the WATEQ4F program, it was determined that predominant species of dissolved Fe in all water samples was Fe²⁺, and those of dissolved Al were AlSO₄ ⁺ and Al³⁺ except for IW2 sample which was associated with white precipitates. The species of dissolved Al in IW2 sample include also AlOH²⁺ and Al(OH)₂ ⁺. The saturation indices of goethite and haematite were positive in the water samples associated with ochrous precipitates (usually called Yellow Boy), therefore these solids might be precipitated. For the IW2 sample, the saturation indices of amorphous Al(OH)₃ and gibbsite were positive, so theoretically these solids might also be precipitated. By XRD analysis, it was found that goethite occurs in ochrous precipitates, and gibbsite in white precipitates.     

测定氨氮的经验点滴

用纳氏比色法测定NH3-N时,在保证斜率不变(b=0.0037)的条件下,减少显色剂中HgCI2-KI三分之二的含量,聚乙烯醇做胶体稳定剂,显著提高了显色剂和显色的稳定度,并大大降低了空白吸光度.以KOH和酒石酸钾纳做缓冲溶液,并增加KOH一倍的含量,保持恒定的显色碱度,同时也掩蔽了金属离子的干扰.测定废水,先做一条件试验,确定氨氮废水的稀释比,是测定氨氮的重要步骤.     

引入稀释因素后的废水处理效果估算方法讨论

讨论了经稀释后废水处理时几种常州的污染物去除率及削减量的估算方法，通过实例分析了各估算方法的区别与联系，并提出了在选用估算方法时的注意事项。