以N,N—二甲基苯胺为偶联试剂示波极谱法测定水中NO2^——N

研究了ＮＯ２＾－－磺胺重氮盐与Ｎ,Ｎ－二甲基苯胺偶联反应的条件及产物在乙醇,ＮＨ３－ＮＨ４Ｃｌ（ｐＨ＝１０）介质中的极谱行为。二阶导数波高与ＮＯ２＾－－Ｎ浓度在０．０００６－０．０７ｍｇ／Ｌ内呈良好线性关系,回收率为９７％－１０２％,已用于环境水中ＮＯ＾－２－Ｎ的测定。     

吸光光度法测定工业污水中NH_4~ —N含量

本法根据ＮＨ＋４与水杨酸在次氯酸钠和亚硝基铁氰化钠的作用下形成一种有色配合物的反应,最大吸收波长为７００ｎｍ,体系中ＮＨ＋４－Ｎ浓度在０～１４μｇ／ｍｌ范围内符合朗伯—比耳定律,测得摩尔吸光系数ε＝１１×１０４。本法灵敏、准确、重现性好,测试误差小于３％,回收率为９６～１０２３１％。     

基于N，N─二甲基苯胺与NO_2~－─对氨基苯磺酸重氮盐的偶联反应示波极谱法测定NO_2~－

报道了利用Ｎ，Ｎ─二甲基苯胺为偶联试剂的Ｃｒｉｅｓｓ反应以示波极谱法测定ＮＯ_２~－的测试方法。在拟定的实验条件下，ＮＯ_２~－在４．０×１０~－３～４．８×１０~－１μｇ／ｍｌ范围内与极谱波波高呈良好的线性关系。环境水测定的相对标准偏差小于ｌ％，回收率在９７％～１０１％之间。     

海河下游水体中DO与NH_3-N、COD_(Mn)相关关系探讨

本文应用近年来海河下游监测数据对ＤＯ与ＮＨ３Ｎ和ＣＯＤＭｎ进行一元线性回归，得到两回归方程：ＮＨ３Ｎ＝－１２８ＤＯ＋１０５４；ＣＯＤＭｎ＝－１１３ＤＯ＋１６９２。并经相关系数和回归系数显著性检验，表明在９９９％的置信水平下ＤＯ与ＮＨ３Ｎ和ＣＯＤＭｎ线性相关均极其显著     

NH_3－N分析中显色后稀释测定误差的探讨

ＮＨ_３－Ｎ分析中显色后稀释测定误差的探讨任晓梅（江苏扬州市环境监测站，扬州２２５）０２）溶液碱度变化影响了纳氏反应平衡，是产生误差的主要原因。稀释５倍时，ｐＨ降低０．５４，误差＜５％；而稀释ＳＯ倍时，与原浓度溶液的ｐＨ值相差１．４，相对误差则高达８?..     

气相色谱法测定废水和废气中N′,N-二甲基甲酰胺

以气相色谱石英毛细管柱分离、ＦＩＤ检测,测定废水和废气中Ｎ′,Ｎ－二甲基甲酰胺（ＤＭＦ）。在１０ｍｇ／Ｌ～１８８１０ｍｇ／Ｌ范围内有良好的线性关系。检测限：废水为０５ｍｇ／Ｌ;废气为０８ｍｇ／ｍ３。样品测定的相对标准差为４％～８％,回收率在７６％～１１２％之间,精密度和准确度均较好     

气相色谱法测定废水和废气中N‘,N—二甲基甲酰胺

以气相色谱石英毛细管柱分离,ＦＩＤ检测,测定废水和废气中Ｎ’,Ｎ－二甲基甲酰胺（ＤＭＦ）,在１．０ｍｇ／Ｌ￣１８８１．０ｍｇ／Ｌ范围内有良好的线性关系,检测限：废水为０．５ｍｇ／Ｌ;废气为０．８ｍｇ／ｍ＾３,样品测定的相对标准差为４％￣８％,回收率在７６％￣１１２％之间,精密度和准确度均较好。     

低浓度二氧化碳检测管的研制

应用活性氧铝—百里香酚酞吸附ＣＯ２线性比长法研制出低浓度ＣＯ２检测管。测定范围０．０５～０．９０％;灵敏度为０．０５％;检测管变色长度与ＣＯ２浓度的相关系数γ＝０．９９８１,精密度与准确度符合国家标准８３ＧＢ７２２０～７２８０。其可靠性与经典的何氏气体分析器比较,结果基本一致。低浓度的ＳＯ２、Ｈ２Ｓ和ＮＨ３对测定无明显干扰,现场监测应用效果可靠,值得推广应用。     

纳氏比色法测定NH_3－N的改进

纳氏比色法测定ＮＨ_３－Ｎ的改进张志贵，古力沙拉（新疆克拉玛依市环境监测站，８３４０００）（１）减少显色剂ＨｇＣ１２、ＫＩ含量，选用２５０ｍｌ含ＨｇＣＩ。３ｇ较适宜，其仅为纳氏法用量的３２％（ＫＩ含量为７．ｓｇ）。（２）以聚乙烯醇做稳定剂，显著提高显?..     

基于8—羟基喹啉与NO^—2—磺胺重氮盐的偶联反应示波极谱法测定NO^—2

研究了８－羟基喹啉与ＮＯ＾－２－碘胺重氮盐偶联反应的条件及其产物的极谱行为。二阶导数波高与ＮＯ＾－２的浓度在０．００２－０．２ｍｇ／Ｌ内呈良好的线性关系,回收率为９８％－１０３％,已用于环境水样中ＮＯ＾－２的测定。     

长春南湖底泥疏浚前后水因子分析及动态变化

监测了长春南湖底泥疏浚后的DO、NH4＿N、NO2＿N、NO3＿N、BOD5、CODCr、TN、TP、SS、pH、SD和水温等12项水化学指标。用因子分析方法找出了底泥疏浚前后影响南湖水质的主要因子,分析了底泥疏浚前后南湖水质变化的特征和底泥疏浚对南湖水质的影响,分析结果表明,南湖疏浚前主要污染物是总磷,疏浚后总磷对水质的影响降低,悬浮物作用增大。     

Spatial distribution of inorganic nitrogen contents of marsh soils in a river floodplain with different flood frequencies from soil-defrozen period

Contents of inorganic nitrogen (NH4(+)-N and NO3(-)-N) in soil profiles were measured in five typical zones ( including permanently flooded floodplain(B), 1-year floodplain (O), 5-year floodplain (F),10-year floodplain (T), and 100-year floodplain (H) )from Huolin River floodplain in Erbaifangzi, Jilin Province of China, in the soil-defrosted period (Mayof 1999). Contour maps and profile maps were constructed to describe the spatial distributions of NH4(+)-N and NO3(-)-N) in order to identify the influences of flood frequencies on them. Results showed that NH4(+)-N generally increased with depth in soil profiles from the five areas, but NH4(+)-N contents in T or H areas significantly differed from those in other areas. For NO3(-)-N, with the exception that there was a significant cumulative peak (6.77 +/- 0.08 mg kg(-1)) at 15-cm depth (10-20 cm) in B area, no significant difference was observed between NO3(-)-N contents in soil profiles from the other four areas. The horizontal distributions of NH4(+)-N and NO3(-)-N in top soils (0-10 cm) were different in the five areas,which were greatly influenced by flood frequencies. The highest content of NH4(+)-N or NO3(-)-N did not appear in B area but in the floodplain with certain flood frequency. For example, NH4(+)-N content (16.81 mg kg-(1)) in 5-year floodplain wetland was highest, and the highest content of NO3(-)-N(1.69 mg kg(-1)) appeared in 1-year floodplain wetland. In addition, NH4(+)-N contents were significantly correlated with soil pH, and NO3(-)-N contents had significant correlation with inorganic carbon, but there were no significant correlations between inorganic nitrogen and other selected soil properties.     

4—（H—酸偶氮）—1—苯基—3—甲基吡唑酮光度法测定铜的研究及应用

合成了新试剂４－（Ｈ－酸偶氮）１－苯基－３－甲基吡唑酮（ＨＰＭＰ）,研究了其和铜的显色反应。在ｐＨ＝７的ＮＨ４Ａｃ缓冲介质中,ＣＴＭＡＢ存在下,ＨＰＭＰ与Ｃｕ（Ⅱ）生成２∶１紫色络合物,λｍａｘ＝５８０ｎｍ,ε＝５．６８×１０４Ｌ·ｍｏｌ－１·ｃｍ－１。铜含量在０～０．６ｍｇ／Ｌ内符合比耳定律。方法用于水样和生物样品中铜的测定,结果令人满意。     

北京市河流氨氮浓度时空演变特征分析

选取2010—2017年北京市地表水监测数据,对河流氨氮(NH 3-N)浓度的时空演变特征进行分析。结果显示,空间上,全市河流NH 3-N浓度整体上保持上游优于下游的分布特征;年均浓度显著下降,由2010年的8.53 mg/L逐年下降至2017年的3.09 mg/L;河流NH 3-N浓度与化学需氧量、总磷呈显著正相关,与溶解氧显著负相关,总氮与NH 3-N的比值随着水质由差到好呈上升状态。污水收集处理和再生水利用是改善北京市河流水质的关键措施。为持续降低河流NH 3-N浓度,改善首都水环境质量,须提高污水处理能力和出水水质,有机结合再生水回用与生态治水理念。     

Contemporary estimates of atmospheric nitrogen deposition to the watersheds of New York State, USA

Atmospheric inputs of reactive nitrogen (N) to ecosystems are a particular concern in the northeastern USA, including New York State, where rates of atmospheric N deposition are among the highest in the nation. We calculate the seasonal and annual spatial variations of contemporary inorganic atmospheric N deposition loading to multi-scale watersheds across New York State using numerous monitoring datasets of precipitation and ambient atmospheric N concentrations. Our models build upon and refine previous efforts estimating the spatial distribution of N deposition. Estimates of total inorganic wet deposition (NH4-N + NO3-N) across New York ranged from 4.7 to 10.5 kg ha(-1) yr(-1) under contemporary conditions (averaged 2002-2004), and both seasonal and annual predicted rates of inorganic N deposition (NH4-N, NO3-N, and total) fit relatively well with that of observed measurements. Our results suggest that "hot spots" of N deposition are, for the most part, spatially distributed according to geographic positions (i.e., relative location from sources and the Great Lakes system) and elevation. We also detect seasonal variations in deposition, showing that total wet atmospheric inorganic N deposition inputs to watersheds (extracted from the four-digit HUC calculations) are highest during the spring (mean = 2.4 kg ha(-1), stddev = 0.29) and lowest during the winter months (mean = 1.4 kg ha(-1), stddev = 0.23). Results also suggest that wet NO3(-) consistently comprises a slightly higher proportion of wet N deposition than wet NH4+ throughout watersheds of New York, ranging from 2.5 to 6.1 kg NO3-N ha(-1) yr(-1) compared to NH4+, which ranges from 2.2 to 4.4 kg NH4-N ha(-1) yr(-1).     

Spatial and temporal variations of nitrogen pollution in Wen-Rui Tang River watershed, Zhejiang, China

Water quality has degraded dramatically in Wen-Rui Tang River watershed, Zhejiang, China, especially due to rapid economic development since 1995. This paper aims to assess spatial and temporal variations of the main pollutants (NH??-N, TN, BOD(5), COD(Mn), DO) of water quality in Wen-Rui Tang River watershed, using the geographic information system, cluster analysis (CA) and principal component analysis (PCA). Results showed that concentrations of BOD(5), COD(Mn), NH??-N, and TN were significantly higher in tertiary rivers than in primary and secondary rivers. From April 2006 to March 2007, the concentrations of NH? ?-N (2.25-57.9 mg/L) and TN (3.78-70.4 mg/L) in all samples exceeded Type V national water quality standards (≥2 mg/L), while 5.3% of all COD(Mn) (1.83-27.5 mg/L) and 33.6% of all BOD(5) (0.34-50.4 mg/L) samples exceeded Type V national water quality standards (COD(Mn)?≥ 15 mg/L, BOD(5)?≥ 10 mg/L). Monthly changes of pollutant concentrations did not show a clear pattern, but correlation analysis indicated that NH??-N and TN in tertiary rivers had a significant negative correlation with 5-day cumulative rainfall and monthly rainfall, while there were no significant correlations in primary and secondary rivers. The results of CA and spatial analysis showed that the northern part of Wen-Rui Tang River watershed was the most seriously polluted. This region is characterized by the high population density and industrial and commercial activities. The PCA and spatial analysis indicated that the degraded water quality is caused by anthropogenic activities and poor wastewater management.     

东江中游水质时空分异特征及影响因素研究

运用多元统计方法，对东江中游水质自动站（河源临江站和惠州剑潭站）2009-2012年水质监测数据进行时空分异特征及影响因素研究。结果表明：水站水质在Ⅰ类～Ⅲ类之间；空间特征差异为 T 与 TB 差异不显著，pH 值、EC、DO、IMn、NH3-N 及 TP均存在极显著差异；水期体征差异为河源临江站除 DO各水期差异显著外，其他指标差异不明显，惠州剑潭站 pH值、EC、IMn与 TP各水期均呈显著差异，NH3-N 水期差异不显著。Pearson 相关性分析表明，T 是制约河源临江站水体 DO的主要相关因子，营养盐作用相对较低；惠州剑潭站水体 DO 与 T、TP及 IMn呈极显著负相关关系。通过因子分析，识别出影响惠州剑潭水质的主因子，量化了水体理化性质、地表径流及人为污染对水质变化的贡献。     

Performance evaluation of a full-scale natural treatment system for nonpoint source and point source pollution removal

This study presents a full-scale performance of a natural treatment system (NTS) facility in Taiwan with nearly 2 years of observations. The study site, composed of several treatment ponds in series, was designed primarily to reduce polluted stormwater runoff from tea gardens and partially to untreated domestic wastewater from nearby villages. Thus, both nonpoint source and point source pollution are treated in this system. From 28 field samplings in 2006-2007, the NTS site shows satisfactory treatment performance and the effluent water quality is significantly improved. Seven of the 28 sampling events are storm events (nonpoint source pollution) and the remainder are from regular monitoring (point source pollution). The average volume of influent and effluent is 533 CMD and 196 CMD, respectively. In order to determine the removal efficiency, several assessment measures are employed in an attempt to obtain unbiased conclusions. They are removal rate (RR), efficiency rate (ER), summation of loads (SOL), flux rate (FR), and effluent probability method (EPM). The average percent removal efficiency of NH(3)-N is 53.5-75.2% and of TP is 59.0-84.7%, in which the highest result is calculated by SOL method and the lowest rate is obtained from RR. In FR evaluation, larger treatment capacity for NH(3)-N than for TP is provided in the site and the average FR is respectively 0.230 g/m(2) day and 0.017 g/m(2) day. Of the methods examined, EPM is the only method capable of illustrating data distribution. Finally, recommendations on the usefulness of these measures are summarized to facilitate the understandings of NTS performance evaluations.     

Effect of nitrogen, potassium and humic acid on 134 Cs transfer factors to wheat from tropical soils in Neubauer growth units

A Neubauer plantlet experiment was carried out using Inceptisol (Typic Haplustept) and Vertisol (Typic Chromustert) soils contaminated with 134Cs at 74 kBq kg(-1) soil to study the transfer factor to wheat crop (Triticum aestivum) as influenced by four levels of humic acid (100, 200, 300, 400 mg HA kg(-1) soil), potassium and NH4-N (36.4, 54.5, 72.7 and 90.9 mg K or NH4 kg(-1) soil) under tropical climate. The biomass yield and K uptake by wheat were significantly improved in Vertisol with NH4-N and K application. The potassium application significantly increased the potassium concentration in wheat plants. The increase in the levels of each of the treatments dramatically improved the yield, K content and K uptake parameters, irrespective of the soils. The 134Cs transfer factors, irrespective of the treatments were observed to be higher in Vertisols as compared to Inceptisols. Among the treatments, the effect of HA was significantly greater than that of K and NH4-N application in Inceptisol, however, in Vertisols both HA and NH4-N were observed to be superior as compared to K application. With each increment in the levels of the treatments, a significantly lowered TF value was found, higher in Inceptisols (56.3%) than Vertisols (48.5%). Comparison of treatments indicates that in general higher potassium concentration in plant drastically lowered radiocesium transfer to wheat. Neubauer plant culture study, a rapid laboratory experimental model based on simple soil-plant system was quite clearly brought out the potential effectiveness of N, K and HA on soil-to-wheat transfer of radiocesium. Such screening technique needs to be extended to cover wider crop species, different climatic conditions and factors governing/modifying the mobility of radiocesium in soil and its absorption by crop plants.