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。     

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。     

不同钝化剂对土壤有效态铅和镉含量的影响

通过向土壤中添加蚕沙、熟石灰和磷酸二氢钾,研究不同钝化处理对土壤有效态重金属含量、pH值及有机质含量的影响.结果表明:添加蚕沙和熟石灰都能使土壤中高植物有效挂的有效态Pb和有效态Cd大幅下降;其中以单施蚕沙处理效果最优,其对Pb和Cd的钝化效率分别达到36.5％和39.2％,而蚕沙+熟石灰处理钝化效果次之,分别为24.3％和26.9％.磷酸二氢钾的钝化作用不明显.添加熟石灰对土壤pH值影响最大,而蚕沙大幅增加了土壤中有机质含量.经统计分析,土壤pH值、有机质含量都与土壤有效态Pb、Cd含量之间呈负相关,说明通过提高土壤pH值及有机质含量,降低土壤重金属活性是土壤重金属钝化的主要机理.     

测定总氮中影响因素的探讨

本文研究了过硫酸钾氧化紫外分光光度法测定总氮的过程中,通过标准曲线、标准物质、具体试样的一系列测定探讨,发现试剂、实验用水、实验器皿、实验环境等对测定结果有很大影响。     

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。     

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。     

高铁酸钾氧化去除弱碱性地下水中低浓度石油类污染物实验研究

研究一般地下水弱碱性水溶液中,高铁酸钾对低浓度石油烃类污染物的氧化去除率.采用0#柴油模拟石油类污染物试验水样,氧化反应在200mL烧杯中模拟完全混合状态完成.实验分析浓度分别为5.02mg/L、2.05mg/L、1.01mg/L和0.52mg/L4个水样石油类污染物氧化去除率.实验研究显示,石油类污染浓度与高铁酸钾浓...     

稀有鮈鲫外周血红细胞微核试验方法研究

将稀有鮈鲫(Gobiocypris rarus)半静态暴露于重铬酸钾溶液中,研究发现稀有鮈鲫的本底微核率处于较低的水平,重铬酸钾在不同浓度和时间暴露后能明显观察到外周血红细胞微核增加。在一定条件下存在剂量-效应关系和时间-效应关系,表明稀有鮈鲫可用于鱼类外周血红细胞微核试验。试验中每尾鱼观察15000个细胞,能有效地减小试验偏差,保证试验结果的可靠性。暴露浓度大于等于0.01mg/L时,染毒组与空白组的外周血红细胞微核率有显著性差异,其微核率随染毒时间的延长呈先升高后下降的趋势,均在24h时出现所有测定时间微核率的峰值。与其他鱼类比较显示,稀有鮈鲫具有较高的敏感性,可用于遗传毒物诱发微核的监测。     

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.