Determination of arsenic in grain and soil by hydride nondispersive atomic fluorescence method

Quantity of trace arsenic in grain and soil was determined by hydride nondispersive atomic fluorescence method.Optimum conditions of measurement were selected in the experiment including the pH of the medium, reductive agent, the concentration and flowing velocity of KBH4, rate of carrier gas and atomized temperature. The reference sample of rice C was determined and the linear relationship of the calibration curve was plotted, indicating that the method was highly precise. In the experiment of recovery rate, the method was quite satisfactory.Based on the determination of hundreds of samples, it is proved that atomic fluorescence method is rapid, sensitive and low in interference. It is very efficient on determination of trace arsenic in soils and grains, especially in grains.     

红壤中结合态磷在酸化条件下的变化及其相互关系

以浙江沿海地区的红壤为研究对象，通过浸滤过程，研究了在酸化条件下，红壤中可溶笥结合态磷的变化和它们之间的相关关系，结果显示，红壤中可溶性Fe-P比Ca－P、Al－P对酸度的变化更为敏感；当红壤中可溶性磷的原始含量较高时，随酸度的增强从固相中释出的趋势更明显；在酸化过程中、红壤中不同可溶性结合态磷之间呈现出不同的相关关系，这归因子它们对酸化敏感性的差异。     

Potential for carbon sequestration in Canadian forests and agroecosystems

The potential for carbon (C) sequestration was examined in selectedCanadian forest settings and prairie agroecosystems under severalmanagement scenarios. A simple C budget model was developed toquantitatively examine C sequestration potential in living biomass of forestecosystems, in associated forest-product C pools, and in displaced fossil-fuelC. A review of previous studies was conducted to examine C sequestrationpotential in prairie agroecosystems. In the forest settings examined, ourwork suggests that substantial C sequestration opportunities can be realizedin the short term through the establishment of protected forest-C reserves.Where stands can be effectively protected from natural disturbance, peaklevels of biomass C storage can exceed that under alternative managementstrategies for 200 years or more. In settings where it is not feasible tomaintain protected forest-C reserves, C sequestration opportunities can berealized through maximum sustained yield management with harvestedbiomass put towards the displacement of fossil fuels. Because there is afinite capacity for C storage in protected forest-C reserves, harvesting forestbiomass and using it to displace the use of fossil fuels, either directlythrough the production of biofuels or indirectly through the production oflong-lived forest products that displace the use of energy-intensive materialssuch as steel or concrete, can provide the greatest opportunity to mitigategreenhouse gas emissions in the long term. In Canadian prairieagroecosystems, modest C sequestration can be realized while enhancingsoil fertility and improving the efficiency of crop production. This can bedone in situations where soil organic C can be enhanced without relianceupon ongoing inputs of nitrogen fertilizer, or where the use of fossil fuelsin agriculture can be reduced. More substantial C offsets can be generatedthrough the production of dedicated energy crops to displace the use offossil fuels. Where afforestation or reconstruction of native prairieecosystems on previously cultivated land is possible, this represents thegreatest opportunity to sequester C on a per unit-area basis. However,these last two strategies involve the removal of land from crop production,and so they are not applicable on as wide a scale as some other Csequestration options which only involve modifications to currentagricultural practices.     

Multimedia model of atrazine in plant-soil-groundwater system with a fugacity approach

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Occurrence and congeners specific of poiychlorinated biphenyls in agricultural soils from Southern Jiangsu, China

A total of 198 agricultural soil samples were collected from Zhangjiagang and Changshu in Southern Jiangsu for analysis of 13 polychlorinated biphenyls (PCBs) in order to assess the levels of pollution, sources, area distribution, and potential risk for the environment. All methods were rigorously tested and an adequate quality control was ensured. Only one site had no PCBs residues, and the highest total PCBs concentration in the surface soils was 32.83 ng/g. The average concentration in all the soil samples was 4.13 ng/g, signaling low-level pollution. Tetra-, penta-, and hexa-chlorinated biphenyls were dominant species in soil samples, accounting for more than 75% ofΣPCBs in the soil samples. PCB118 was the most abundant congener in all the samples. The PCB118 was about 20% ofΣPCBs. The soil organic matter content showed only a weak correlation with the levels of all PCB congeners, in which a better correlation was noted for the more volatile lighter PCB congeners than for the heavier homologues. To a certain extent, the sources and land use seemed to influence the levels of PCBs.     

土壤环境容量数学模型——Ⅰ.土壤污染动力学模型

应用物质平衡原理,导出模拟土壤污染过程的动力学方程.可用于估算土壤环境容量、分析土壤污染动态和预测土壤超容年限.以测定残留率为基础的一类模型是本文提出的模型的一个特例.     

和田绿洲沙尘暴物质输送路径及其对大气环境质量的影响

为了研究来自不同方向的沙尘暴对和田绿洲大气环境质量的影响，本文利用HYSPLIT后向轨迹模型和NCEP的GDAS全球气象要素数据，将和田绿洲西北部的墨玉县城作为模拟受点（37.26°N，79.72°E），计算2016年1月1日—2018年12月31日发生的每一次沙尘天气期间逐日18：00（世界时）36 h后向气流轨迹，轨迹计算起始高度设置为500 m，并结合相应的PM_2.5、PM₁₀、SO₂、NO₂、CO、O₃浓度监测数据进行聚类分析，研究抵达该地区的沙尘暴的主要移动轨迹和污染物输送路径.同时，运用潜在源贡献因子分析法（PSCF）和权重污染轨迹分析法，分析了沙尘暴期间不同气流轨迹对墨玉县污染物浓度的影响，识别大气污染物的潜在源区，揭示不同源区对污染物浓度的贡献差异.结果表明，影响和田绿洲（墨玉县）的沙尘暴主要来自西北（WN）、北（N）、东北（EN）和东（E）4个方向；其中，来自东部的沙尘天气频率最高（60.2%），但主要以浮尘天气为主；扬沙和强沙尘暴主要来自西部方向，54.48%的强沙尘暴和38.53%的扬沙来自西和西北方向.不同沙尘源区和不同传输路径上的沙尘气溶胶对和田绿洲大气环境的影响不一样.沙尘天气期间，大气PM_2.5和PM₁₀的平均浓度相当于无沙尘天气期间的3~5倍，但对SO₂、NO₂、CO、O₃质量浓度的影响不大；由西向东和由北向南的沙尘暴对墨玉县PM_2.5和PM₁₀质量浓度的贡献率最大；由东向西的沙尘暴由于路过和田市和洛浦县等工业污染源区，此簇沙尘暴气团将该区域SO₂、NO₂、CO等污染颗粒携带到墨玉县，因此，东-东南（E-ES）方向的沙尘暴对SO₂、NO₂、CO的贡献率分别为15.56%、20.55%和21.57%.本文定量印证了沙尘暴对和田绿洲大气环境质量的影响，可为绿洲区沙尘暴研究提供参考.     

Effect of acid precipitation on leaching of nutritionsand aluminium from forest soils

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生物质炭对Cd污染土壤团聚体酶活性的影响

为探究生物质炭对Cd污染土壤团聚体酶活性的影响,采用盆栽试验,向模拟Cd污染土壤中添加生物质炭并测定水稻根际土壤团聚体碳循环酶与氧化还原酶活性.结果表明:Cd污染土壤团聚体酶活性对添加量为2.5%的生物质炭响应明显,氧化还原酶活性指数值介于0.522~0.792之间.在2.5mg/kg的外源Cd条件下,2.5%的生物质炭比未添加生物质炭处理显著提高蛋白酶与过氧化氢酶活性至121%与653%.在Cd污染土壤中添加生物质炭,碳循环酶与氧化还原酶及综合酶活性均在0.5~1mm中等粒径土壤团聚体中产生富集效应,其酶活性随土壤团聚体粒径的增大呈先升后降最终趋于稳定的趋势.研究显示,在2.5mg/kg的外源Cd条件下,添加2.5%的生物质炭对水稻根际土壤团聚体酶活性影响显著,土壤酶活性受酶种类、生物质炭量与团聚体粒径的综合影响;在Cd污染土壤中添加生物质炭后,土壤酶活性随团聚体粒径的增大呈“∧”形变动规律.     

川西北草原土壤硼、锰丰缺状况初探

根据110余个表层土壤样品硼、锰含量的测定结果和土壤缺乏硼、锰的临界值指标,探究了川西北草原土壤中硼、锰的有效性及其丰缺状况.结果表明,本区土壤中全硼全锰含量丰富分别达166.0ppm和736.6ppm,但有效硼和锰的含量仅分别为0.45ppm和5.11ppm,土壤缺乏硼和锰比较普遍.为该区推广施用硼、锰微肥提供了初步的科学依据.