钯离子液相催化氧化低浓度磷化氢

采用Pd^2＋液相催化氧化低浓度PH3,考察了Pd^2＋浓度、O2体积分数、PH3质量浓度、混合气流量、反应温度等因素对Pd^2＋吸收液去除低浓度PH3效果的影响。实验结果表明,采用10mL Pd^2＋浓度为0．112mol／L的水溶液作为吸收液净化含低浓度PH3的混合气,在反应温度22℃、O2体积分数5％、PH3质量浓度850mg／m^3、混合气流量190mL／min的条件下,印min之内PH3去除率保持在90％以上。Pd^2＋浓度越高、O2体积分数越大、反应温度越高,PH3去除率越高;混合气流量越大,PH3去除率越低;反应温度越低、O2体积分数越大,PH3去除率的下降速率越小。     

准液膜富集环境水中痕量金属离子

对准液膜法富集环境水中痕量Ｚｎ２＋、Ｃｄ２＋、Ｐｂ２＋进行了研究,此法简单、快速,富集倍数达１００倍,回收率在９５％以上。     

延边地区水稻稳产高产施肥体系的探讨

采用二次饱和D-最优设计,建立了有机肥、氮肥、磷肥和钾肥配合施用对水稻产量影响的数学模型.研究表明有机肥施用量的过多或过少均使水稻产量下降,化肥的施用也有相似的影响;有机肥与氮肥、磷肥、钾肥只有施用量在适宜的范围内,交互作用较大,产量最高.提出了延边地区水稻获得稳产、高产的施肥体系.     

高效液相色谱-电喷雾离子源-串联三重四极杆质谱法分析地表水中高氯酸盐

建立了高效液相色谱-电喷雾离子源-串联三重四极杆质谱(HPLC-ESI-MS/MS)测定地表水中高氯酸盐的方法。以Dionex IonPac AG20阴离子交换柱为分析柱,弱碱性的0.056%氨水/5 mmol/L乙酸氨为流动相,1.0 mL/min的流速,电喷雾负离子模式电离,MS/MS串联质谱为检测器,多反应监测(MRM)模式检测高氯酸盐。方法检出限达0.043μg/L,线性范围为0.2~50μg/L,线性相关系数为0.999 4,含量分别约为2、6、30μg/L的实际样品进样10次得到的相对标准偏差分别为2.47%、4.55%、0.49%,样品加标回收率在80%~109%,将该法与US EPA method314.0进行比对,结果基本吻合。     

渤海湾入海溶解无机氮总量控制研究

基于渤海湾近岸海域的实际调查结果,采取生态物理耦合模型,对渤海湾的主要污染物-溶解无机氮(DIN)的基准环境容量和极小剩余海洋环境容量进行了计算。结果表明,渤海湾DIN的极小剩余海洋环境容量在Ⅰ类和Ⅱ类水质标准下均为负值,渤海湾的DIN已经超标。结合实际的海水功能区水质管理目标,应重点控制非点源的排放,加强上游携带入境污染物的处理,从总量上控制DIN入海污染通量,改善渤海湾水质。     

新疆阜康冶炼厂无污染工艺及环境治理

介绍了阜康冶炼厂无污染新工艺和环境治理的有关情况 ,从理论上阐述了无污染工艺和污水治理的技术原理 ,对有色金属冶炼工业逐步采用湿法精炼清洁工艺有一定的指导作用     

天津市PM2.5中水溶性无机离子污染特征及来源分析

2008年1、4、7月和10月在天津大气层边界站,利用中流量采样器对大气中的细粒子进行了滤膜样品采集,应用离子色谱检测技术分析了8种水溶性无机离子(Na⁺、NH₄⁺、K⁺、Mg²⁺、Ca²⁺、SO₄^2-、NO₃^-和Cl^-)的含量。结果表明,天津市大气PM_2.5中总水溶性无机离子平均浓度为47.3 μg/m³,其中,SO₄^2-、NO₃^-、NH₄⁺和Cl^-是最主要的水溶性无机离子,占总离子质量分数共计87.3%,表明了天津市细粒子中的主要水溶性无机离子的特征。/2 平均比值接近1.0,显示硫酸氨是细粒子中硫酸盐的主要存在形式。NO₃^-/SO₄^2-浓度比的平均值为0.65,反映了燃煤污染与机动车尾气污染并存的复合型大气污染特征。并通过对PM_2.5中8个水溶性离子成分的主成分分析进一步揭示了其来源。     

Synthesis of hydrogarnet from molten slag and its hydrogen chloride fixation performance at high temperature

Hydrogarnet was synthesized hydrothermally below 200°C using molten slag obtained from municipal solid waste. For comparison, it was also synthesized using pure-phase CaO–Al₂O₃–SiO₂–H₂O, as reported previously. The structural and textural properties of this material were investigated using various analytical and spectroscopic techniques such as X-ray diffraction, X-ray fluorescence spectrometry, atomic absorption spectrometry (AAS), thermogravimetry/differential thermal analysis, Fourier transform infrared spectroscopy, and scanning electron microscopy. The Cl⁻ fixation ability of hydrogarnet was investigated in the temperature range 500–800°C in a fixed-bed flow reactor using a HCl concentration (1000 p.p.m.v.) similar to that of incinerator exhaust gas. Under these experimental conditions, the hydrogarnet was capable of reducing the HCl gas level to less than 1 p.p.m.v. Analysis of the spent catalyst revealed that the hydrogarnet was being transformed into wadalite and CaCl₂ at high temperatures. The elution test for chromium ions in hydrogarnet obtained from slag was also used, and it was found that chromium ions were not eluted from hydrogarnet. Received: January 27, 2001 / Accepted: October 11, 2001     

城市土地资产经营新思路探讨

自1996年上海市成立第一家土地收购储备机构——土地发展中心后，全国各大城市已纷纷效仿它的成功经验。截止2001年8月不完全统计，全国已有大小不同的土地收购储备机构669家。实践证明，土地收购储备机制在盘活城市存量土地，促进土地集约利用，保障城市土地资产的保值增值等方面成绩卓著。然而，实践过程中，土地收购储备机制的运作也暴露出不少问题。本文通过对这些问题的分析，提出了引进公司制度完善土地收购储备机制，合理运营城市土地资产的新思路。     

Response of Organic and Inorganic Carbon and Nitrogen to Long-Term Grazing of the Shortgrass Steppe

We investigated the influence of long-term (56 years) grazing on organic and inorganic carbon (C) and nitrogen (N) contents of the plant–soil system (to 90 cm depth) in shortgrass steppe of northeastern Colorado. Grazing treatments included continuous season-long (May–October) grazing by yearling heifers at heavy (60–75% utilization) and light (20–35% utilization) stocking rates, and nongrazed exclosures. The heavy stocking rate resulted in a plant community that was dominated (75% of biomass production) by the C₄ grass blue grama (Bouteloua gracilis), whereas excluding livestock grazing increased the production of C₃ grasses and prickly pear cactus (Opuntia polycantha). Soil organic C (SOC) and organic N were not significantly different between the light grazing and nongrazed treatments, whereas the heavy grazing treatment was 7.5 Mg ha^–1 higher in SOC than the nongrazed treatment. Lower ratios of net mineralized N to total organic N in both grazed compared to nongrazed treatments suggest that long-term grazing decreased the readily mineralizable fraction of soil organic matter. Heavy grazing affected soil inorganic C (SIC) more than the SOC. The heavy grazing treatment was 23.8 Mg ha^–1 higher in total soil C (0–90 cm) than the nongrazed treatment, with 68% (16.3 Mg ha^–1) attributable to higher SIC, and 32% (7.5 Mg ha^–1) to higher SOC. These results emphasize the importance in semiarid and arid ecosystems of including inorganic C in assessments of the mass and distribution of plant–soil C and in evaluations of the impacts of grazing management on C sequestration.