HBCOD-1型COD在线自动监测仪的应用

介绍了HBCOD-1型COD在线自动监测仪的测定原理、分析流程和性能特点。仪器采用重铬酸钾氧化水中有机物和还原性无机物，通过分光光度法测定水中化学耗氧量（COD值）。与国标方法进行线性回归校正后，仪器测定值与国标方法测得的CODCr，值具有较好的一致性。     

重铬酸钾法测定化学需氧量的几点体会

重铬酸钾法是测定工业废水中化学需氧量的国家标准方法，通过大量的实验对CODCr的实验进行探索，提出几点体会，在CODCr的测定中有一定的实用性。     

废水中含磷表面活性剂的测定

应用非水电位滴定法测定了废水中各种烷基磷酸酯钾盐及其单、双酯盐。方法的变异系数分别为２．３％和７．８％（ｎ＝１２）。本法可有效地消除非离子表面活性剂的干扰，适用于化纤油剂的质量检验和上油槽中油剂浓度的测定。     

MERCK公司COD试剂的替代品开发

德国MERCK公司制造的COD测定仪器在我国环保行业、科研院所的水质监测工作中应用广泛,但配套试剂价格昂贵,限制了该仪器的使用。实验设计了高量程(100～1500mg/L)和低量程(25～100mg/L)COD替代试剂的开发方案。通过实验,确定了两个量程下COD替代试剂中K2Cr2O7、H2SO4-Ag2SO4、HgSO4的浓度和投加量以及测试方法。实验结果表明,在高量程和低量程范围内,使用COD替代试剂的测试结果与MERCK公司配套试剂的测试结果比较相符,反应时间也可缩短至30min。     

水中总氮空白的影响因素的探讨

本研究以水中总氮空白值为研究对象,不同厂家的过硫酸钾和不同试验用水条件下的总氮空白的变化规律。研究结果表明：无氨水和二次水蒸出来的总氮空白明显低于一次水蒸出来的总氮空白;这跟蒸馏水纯度有关系,一次水含有氨,所以消解时蒸馏水中的氨会被氧化,从而导致空白值偏高。同样有的厂家的过硫酸钾纯度不高,所以导致空白值高。     

空白值校正法无汞快速测定地表水化学需氧量

探讨了K2Cr2O7在不同酸度的硫酸介质中的化学行为,确定9 mol/L H2SO4为K2Cr2O7法测定地表水COD的合理酸度。多种有机物消解试验及半年多地表水样跟踪检测,将消解回流时间从2小时缩短到30分钟之内是可行的。氯离子(Cl-)干扰可用生成AgCl沉淀和空白值校正的办法消除。此方法的检出下限是11mg/L,样品测定的加标回收率在96%～101%。此方法不仅缩短了回流时间、减少了汞带来的二次污染,从而实现无汞快速测定地表水COD。     

水质测定中高锰酸盐指数(酸性法)影响因素的研究

探讨了水质测定中酸性法高锰酸盐指数的影响因素:加热时间、加热温度、溶液浓度、滴定速度、水样酸度,掌握了最佳试验条件,使测定结果更准确。     

不同来源废水COD、TOC与Cl-的关系

通过对含盐化工废水(A)、受潮汐影响的河流水(B)、城市生活污水处理厂排水(C)、采油废水(D)4种不同来源废水进行为期15 d的采样监测,测定了其COD、TOC和Cl-浓度,分析比较了3种废水指标之间的关系,其中COD分别使用重铬酸钾法、氯气校正法和碘化钾碱性高锰酸钾法3种方法进行测定.实验结果表明,4种废水Cl-浓...     

Long-term depletion of calcium and other nutrients in eastern US forests

Both harvest removal and leaching losses can deplete nutrient capital in forests, but their combined long-term effects have not been assessed previously. We estimated changes in total soil and biomass N, Ca, K, Mg, and P over 120 years from published data for a spruce-fir site in Maine, two northern hardwood sites in New Hampshire, central hardwood sites in Connecticut and Tennessee, and a loblolly pine site in Tennessee. For N, atmospheric inputs counterbalance the outputs, and there is little long-term change on most sites. For K, Mg, and P, the total pool may decrease by 2%–10% in 120 years depending on site and harvest intensity. For Ca, net leaching loss is 4–16 kg/ha/yr in mature forests, and whole-tree harvest removes 200–1100 kg/ha. Such leaching loss and harvest removal could reduce total soil and biomass Ca by 20%–60% in only 120 years. We estimated unmeasured Ca inputs from rock breakdown, root-zone deepening, and dry deposition; these should not be expected to make up the Ca deficit. Acid precipitation may be the cause of current high leaching of Ca. Although Ca deficiency does not generally occur now in acid forest soils, it seems likely if anthropogenic leaching and intensive harvest removal continue.     

Soil microbial response to waste potassium silicate drilling fluid

Potassium silicate drilling fluids (PSDF) are a waste product of the oil and gas industry with potential for use in land reclamation. Few studies have examined the influence of PSDF on abundance and composition of soil bacteria and fungi. Soils from three representative locations for PSDF application in Alberta, Canada, with clay loam, loam and sand textures were studied with applications of unused, used once and used twice PSDF. For all three soils, applying ≥ 40 m³/ha of used PSDF significantly affected the existing soil microbial flora. No microbiota was detected in unused PSDF without soil. Adding used PSDF to soil significantly increased total fungal and aerobic bacterial colony forming units in dilution plate counts, and anaerobic denitrifying bacteria numbers in serial growth experiments. Used PSDF altered bacterial and fungal colony forming unit ratios of all three soils.