铝、铁共聚作用的化学特征及晶貌研究

通过对铝，铁水解共聚物的合成制备及其水解共聚合过程电位滴定的研究，并通过扫描电镜对其共聚物样品的晶貌观测，ｎＡｌ／ｎＦｅ的点能谱及结构组成的红外光谱测定，对铝铁共聚作用的化学特征及其晶形貌象，共聚作用进行了研究及讨论，为深入研究铝无机共聚溶液体系化学形态组成及其絮凝剂的提供了的基础实验依据。     

Effect of long-term fertilization on soil nitrate distribution

ＩｎｔｒｏｄｕｃｔｉｏｎＦｅｒｔｉｌｉｚａｔｉｏｎｉｓｅｓｓｅｎｔｉａｌｆｏｒａｇｒｉｃｕｌｔｕｒａｌｐｒｏｄｕｃｔｉｏｎ ,ｂｕｔｕｎｒｅａｓｏｎａｂｌｙａｐｐｌｙｉｎｇｆｅｒｔｉｌｉｚｅｒｓｃｏｕｌｄｒｅｓｕｌｔｉｎｓｅｒｉｅｓｏｆｐｒｏｂｌｅｍｓｓｕｃｈａｓｃｒｏｐｑｕａｌｉｔｙｄｅｃｌｉｎｅ,ｆｅｒｔｉｌｉｚｅｒｕｓｅｅｆｆｉｃｉｅｎｃｙｄｅｃｒｅａｓｅ,ｒｅｓｉｄｕａｌｆｅｒｔｉｌｉｚｅｒｓｐｏｌｌｕｔｉｏｎ ｇｒｏｕｎｄｗａｔｅｒａｎｄｒｉｖｅｒｓａｎｄｎｉｔｒｏｇｅｎｃｏｎｔｅｎｔｅｄ …     

锌镉还原法的海水硝酸盐浓度

按照《海洋调查规范》(1991)中锌镉还原法 ,用三对基体来配制NO3 -标准溶液 :NaCl水 (31gNaCl加纯水至 1L)与无氮东海海水ECS、《海洋调查规范》(1991)人工海水SAS(NaCl水加MgSO4)与ECS和Strick land Parsons(1972 )人工海水SP72 (SAS加NaHCO3 )与ECS。经测定 ,且忽略标准曲线方程的截距 ,纯水与ECS的NO3 -还原率比为 0 .2 6 6 ,NaCl水与ECS的比为 0 .70 6 ,SAS与ECS的比为 0 .90 1,而SP72与ECS的比则为1.0 0 9。显然 ,用ECS和等价的SP72定出的值最接近天然海水中NO3 -的浓度。由《海洋调查规范》(1991)SAS定出的浓度须乘上 0 .90 1～ 0 .95 6后才接近海水中NO3 -浓度。     

硝酸银滴定法与硫氰酸汞分光光度法测定水中氯化物（Cl^-）的方法比对

用硝酸银滴定法、硫氰酸汞分光光度法分别测定高浓度的考核已知样及低浓度的考核未知样，均合格。说明两种方法都能满足水和废水中氯化物（Cl^-）测定的需要。     

以工业废物制备高效氧化铁系脱硫剂的研究

研究了以硫酸烧渣、转炉赤泥、平炉尘为主要原料制备氧化铁系 (SW型 )脱硫剂的方法及制备工艺。结果表明 :脱硫剂最佳配方为粘结剂 5 %～ 8% ,制孔剂 0 0 8%～ 0 1% ,木屑 8%～ 12 % ,工业废渣 (硫酸烧渣、转炉赤泥、平炉尘等 ) 78%～ 88% ;成型的最佳温度为 15 0℃ ,活化方法应根据主要原料的不同有所差异 ,活化条件以成型活化优于成型前活化     

聚合硫酸铁和聚合硫酸铝的配伍和性能研究

将聚合硫酸铁 (PFS)与聚合硫酸铝 (PAS)按一定比例混合 ,即可制得一类具有不同铝铁含量的新型净水剂——聚合硫酸铁铝 (PFAS)混合液 ,分析、检测了几种 PFAS的性质及其净水性能。结果表明 ,PFAS的综合性能优于 PFS和PAS,更能适应原水水质的变化 ,其中尤以铝铁分子摩尔比为 0 .64的 PFAS性能最优。     

Field measurements of dissociation of ammonium nitrate at a Beijing site

ＦｉｅｌｄｍｅａｓｕｒｅｍｅｎｔｓｏｆｄｉｓｏｃｉａｔｉｏｎｏｆａｍｍｏｎｉｕｍｎｉｔｒａｔｅａｔａＢｅｉｊｉｎｇｓｉｔｅＳｈｅｎＪｉ，ＺｈａｏＱｉａｎｘｕｅＲｅｓｅａｒｃｈＣｅｎｔｅｒｆｏｒＥｃｏＥｎｖｉｒｏｎｍｅｎｔａｌＳｃｉｅｎｃｅｓ，Ｃ...     

PREDICTIVE MODEL FOR NITRATE LOAD IN THE BULL RUN WATERSHED,OREGON1

ABSTRACT: Predictive models for nitrate in four streams in the Bull Run Watershed in the Cascade Mountains of Oregon were developed from a record of 17 years of nitrate samples. The models are time series regression models written in terms of Log(nitrate load). The independent variables are logarithm of 14-day mean daily stream discharge, current day's precipitation, logarithm of the previous day's precipitation, total precipitation for the previous seven days, a hydrograph position variable that indicates rising or falling limb, and average maximum air temperature for the preceding 14 days. The models describe annual cycle and seasonable trends and variations in nitrate load, but are unable to describe large day to day variations like those associated with hydrograph peaks.     

硝酸甲胺反应过程的安全性研究

用反应量热仪(RC1e)对硝酸溶液与一甲胺溶液在反应过程中的热安定性进行初步研究,分别测试不同反应温度、加料速度和初始硝酸浓度下反应的放热情况。实验结果表明:该中和过程反应迅速,在室温就能进行;与反应温度、加料速度相比,起始硝酸浓度对反应安全性影响最大,且硝酸浓度越高,反应的速度和反应的完全程度也越高。实验还表明:RC1e是研究反应过程中热安定性情况的有效工具,能通过反应过程的热量变化体现反应速率,所得结果对硝酸甲胺的工业化生产具有重要的参考价值。     

Rapid amino acid cycling in arctic and antarctic soils

Amino acids constitute one of the largest inputs of organic nitrogen (N) to most polar soils and have been hypothesized to be important in regulating vegetational succession and productivity in Arctic ecosystems. Our understanding of amino acid cycling in these soils, however, is poor. The aim of this study was to investigate the size and rate of turnover of the amino acid pool in a range of Arctic and Antarctic soils. Our results indicate that in polar soils with either high or low ornithogenic inputs the amino acid pool is small in comparison to the inorganic N pool (NO^–₃ and NH⁺₄). The free amino acid pool constituted only a small proportion of the total dissolved organic nitrogen (DON) pool in these soils. Here we show that these low concentrations may be due to rapid use by the soil microbial community in both Arctic and Antarctic soils. The turnover of the amino acid pool in soil was extremely rapid, with a half-life ranging from 2 to 24 h, indicating that this N pool can be turned over many hundred times each summer when polar soils are frequently unfrozen. The implications of amino acids in N cycling and plant and microbial nutrition are discussed.