煤中碘的淋滤行为研究

用不同pH值溶液对煤进行动态淋滤实验,用电感耦合等离子体质谱(ICP-MS)测定不同pH值淋滤液在不同时间段获取的淋出液中碘的浓度,以及煤和淋滤后残留煤的高温热水解溶液中碘的含量。结果表明,淋滤液pH值、淋滤时间、煤中碘的赋存形态及在煤中的赋存部位对碘的淋出有重要影响。淋滤液的酸性越强,煤中碘的淋出越多,pH值为2.0和pH值为4.0溶液对煤中碘的淋出率(η)分别为7.22%和6.20%;但pH值为2.0溶液的淋出液中碘的量小于pH值为4.0溶液的淋出液中碘的量,其百分率(w_x)分别为1.920 0%和5.420 0%。pH 2.0淋滤液,在前30 h内淋出液中碘的平均浓度为10.9 μg/L;而pH值为4.0淋滤液,在前110 h内淋出液中碘的平均浓度为10.6 μg/L;pH值为6.0和pH值为7.5溶液能淋出煤中碘很少。在酸性溶液作用下,首先被淋出的碘是存在煤颗粒表面少量的水溶态和离子交换态碘及大部分碳酸盐态和铁锰氧化物结合态碘,然后煤基质内部的部分水溶态和离子交换态碘及少量的碳酸盐结合态及铁锰氧化物结合态碘等才被淋出。     

无烟煤中碘燃烧释放和转化行为研究

采用逐级化学提取法研究无烟煤及其不同温度燃烧产物中碘的各种赋存状态;以小型管式炉模拟煤燃烧装置,考察了加热温度、加热时间、O_2流量以及通入水蒸气对无烟煤中不同形态碘燃烧释放影响及其机理。结果表明,无烟煤中碘主要以有机结合态、铁锰氧化物结合态和水溶态形式存在。加热温度对碘释放和转化有明显影响,碘释放率随温度升高而增加,500-900℃是碘释放的主要阶段。其中,700℃以前,水溶态、离子交换态和有机结合态碘大部分释放,小部分转化为碳酸盐结合态、铁锰氧化物结合态和残留态碘;铁锰氧化物结合态碘主要在700-900℃释放,部分残留态碘在1 100℃前也可释放。无烟煤中碘释放率随燃烧时间延长和O_2流量增大而增大,水蒸气的参与能明显促进碘的释放。在1 100℃、通入水蒸气、O_2流量120 m L/min、燃烧20 min时,93.8%-95.9%碘主要以HI和I_2释放。     

土壤样品中砷的形态分析方法研究

对生态地球化学土壤样品,在Tessier修正顺序提取方法(即七步法)的基础上对提取方法、提取时间、提取溶液的处理方法进行优化选择,用超声法提取水溶态、离子交换态、碳酸盐结合态、腐殖酸结合态、铁锰氧化物结合态、强有机质结合态和残渣态七种形态的砷元素,用原子荧光光谱法测定各个形态砷的含量。优化后的方法测得As元素各形态的检出限均小于1.0μg/g,相对标准偏差(RSD)小于10%,准确度高,质量参数均满足生态地球化学土壤样品评价形态分析的需要。     

成都经济生态区大气降尘中镉赋存形态的研究

采用Tessier连续提取法对成都经济生态区不同区域的24个大气降尘样中镉的赋存形态进行了研究。研究结果表明,大气降尘中的镉主要以残留态形态存在;各形态镉在总镉中所占百分比含量由大到小排列顺序依次是:残留态,碳酸盐结合态,交换态,铁锰结合态,有机结合态;交换态镉、碳酸盐结合态镉这两种具有较高生物有效性的形态镉在总镉中所占的平均百分比含量分别是6.420%和8.917%;铁锰氧化物结合态、有机结合态、残留态镉这三种形态镉生物有效性很低,分别在总镉中所占的平均百分比含量分别是3.419%、2.365%和78.907%。通过分析可得出,汽油和煤的燃烧以及工厂排放镉能加大城市大气降尘的镉污染。     

煤中溴的淋滤行为研究

在不同pH值条件下对来自重庆磨心坡矿煤样进行柱淋滤实验,用电感耦合等离子体质谱法( ICP-MS )测定煤中溴的含量及四种淋滤介质在不同时间段获取的淋出液中溴的浓度。结果表明,淋滤液的pH值、淋滤时间、煤中溴的赋存形态及在煤中赋存部位对溴的淋出有重要影响。淋滤液的酸性越强,煤中溴的最大淋出浓度越大,一定时间内溴的总淋出率也越高。 pH值为2的淋滤液,在淋滤前40h内淋出溴的量占总淋出量的80.65%;pH值为4的淋滤液,在淋滤前50h内淋出溴的量占总淋出量的89.42%。在酸性淋滤液作用下,首先被淋出的是存在煤颗粒表面的碳酸盐态和铁锰结合态溴,然后煤基质内部的水溶态和离子交换态溴才被淋出。柱淋滤实验表明,煤中溴在风化过程中,会被酸性雨水淋溶出来进入周围土壤或地表水体,造成周围环境溴的富集。     

氢化物发生原子荧光法测定稻田土中的锑形态

采用王水消解及逐级浸提技术,以氢化物发生-原子荧光法对成都东郊稻田土中的Sb形态进行了分析,方法检出限为0.108μg/L,回收率为96.9%～104.8%。加入硫脲-抗坏血酸溶液后,土壤样品中可能存在的金属离子Cu2+、Co2+、Se4+、Sn2+、Zn2+、Pb2+、As3+、As5+、Hg2+对Sb的干扰可以有效地消除;样品Sb含量在0.92～2.52 mg/kg之间波动,平均值为1.76 mg/kg,与四川省土壤Sb背景浓度(≈1.70 mg/kg,1991)相比相差不大。水平方向上,各形态Sb的浓度因所处稻田条件的不同而分布各异,大体呈以下规律:残渣态﹥有机/硫化物结合态﹥铁/锰氧化物结合态﹥碳酸盐结合态﹥可交换态,易被植物吸收利用的可交换态占的比率最小;垂直方向上,各形态随着土壤深度的增加,呈递减趋势。     

柱层析分离—原子吸收法测定麻叶千里光有机态和无机态中微量元素硒

通过柱层析分离,首先采用氯仿分离麻叶千里光有机态和无机态;然后选择正己烷等3种不同极性溶剂作洗脱剂,以硅胶柱进行洗脱;最后用石墨炉原子吸收分光光度计测定了麻叶千里光各洗脱液中硒的含量。结果表明,麻叶千里光有机态和无机态经过正己烷、乙酸乙酯、甲醇3种不同极性溶剂洗脱,测得硒元素含量存在显著差异,其中有机态洗脱后,硒元素含量分别为:正己烷5.142μg/g,乙酸乙酯3.329μg/g,甲醇2.011μg/g;而无机态洗脱后,测得硒元素含量分别为:正己烷1.956μg/g,乙酸乙酯2.505μg/g,甲醇4.109μg/g;RSD(%)分别为:有机态-正己烷0.66,有机态-乙酸乙酯1.04,有机态-甲醇0.38,无机态-正己烷0.42,无机态-乙酸乙酯0.80,无机态-甲醇0.58;加标回收率分别为:98.79%,99.76%,91.42%,82.99%,102.2%,94.50%。     

连续浸提-分光光度法测定硼泥中不同形态的硼

采用连续浸提法将硼泥中的硼划分为七种物理形态,即:水溶态、醇溶态、盐溶态、络合态、硫酸盐等结合态、Fe-Mn结合态及残渣态。用分光光度法测定各形态硼的含量。测定结果的相对标准偏差为4.4%(n=4),回收率为91.7%~102.4%。     

可溶性有机质对污染土壤中铊迁移行为的影响

目的 为了查明可溶性有机质（DOM）对土壤中污染元素铊赋存形态的影响,方法 采用形态分级提取方法,将土壤中的铊重金属分成酸可交换态、铁锰氧化物结合态、有机质结合态和残留态4组分,并采用Elan 6100型ICP-MS质谱仪测定各组分中铊的质量浓度.结果 DOM可降低酸可交换态的Tl,增加铁锰氧化物结合态和有机质结合态Tl的百分含量,但对残留态Tl的百分含量没有明显影响.因此,DOM可降低铊在土壤中的活动性,从而改变了铊在土壤中的迁移行为.结论 可溶性有机质（DOM）自身的络合（螯合）能力及其吸附特性是改变重金属铊形态分布的主要因素.     

原子吸收光谱法测定烟叶中的重金属总量及形态分析

采用火焰原子吸收光谱法测定烟叶中Mn,Cu,Zn元素,石墨炉原子吸收光谱法测定Cd,Cr,Pb元素,以HNO3-H2O2微波消解法获取烟叶中的重金属总量,以超声水提取法获取水溶态重金属进行初级形态分析,以Tessier逐级提取法获取5种形态的重金属进行次级形态分析。实验结果表明,原子吸收光谱法检测6种重金属线性良好,相关系数(r2)不低于0.998 8,检出限为0.16~3.1μg·L-1。烟叶样品中Mn,Cu,Zn,Cd元素主要以可交换态和碳酸盐结合态的形式存在;Cr主要以残渣态的形式存在;而Pb主要以碳酸盐结合态和残渣态的形式存在。     

煤中氯在亚临界水条件下的变迁

运用半连续反应装置对山西吴家坪煤和四川华蓥山煤中氯在亚临界水条件下的脱除规律及形态变化进行了研究。考察了反应温度和压力对氯脱除率的影响；同时还运用化学提取法对原煤及残渣中氯的形态进行了研究。研究结果表明,随着反应温度的升高，煤中氯的脱除率也增加，在410℃、15MPa、60min、水流量为580mL/h时，吴家坪煤中氯的脱除率为84.6%，华蓥山煤中氯的脱除率为72.4%。吴家坪煤中氯在15MPa时的脱除率最大。华蓥山煤中氯主要以有机氯的形态存在，而吴家坪煤中氯有8%为离子可交换态的无机氯，其余为有机结合的氯；在亚临界水萃取煤的过程中，离子交换态结合的有机氯比共价键结合的有机氯更容易挥发,有机氯要首先转化为无机氯然后再逸出。     

Preparation and characterization of colloidal dispersions of graphene-like structures from different ranks of coals

This paper focuses on preparation of colloidal solution of graphene-like structures from different ranks of coals: brown coal, bituminous coal, low-volatile bituminous coal, anthracite. It was found that brown coal thermo-oxidative destruction leads to formation of small d=32 nm (V=17%) and large d=122 nm (V=11%) fractions of nanoparticles. The thermo-oxidative destruction of bituminous coal leads to formation of nanoparticles d=50 nm (V= 5.2%) and d=164 nm (V=16%). Thermo-oxidative destruction of low-volatile bituminous coal and anthracite leads to formation of nanoparticles, predominantly, d= 122-190 nm. Carbon nanostructures obtained from coal are negatively charged at pH=2-12. Colloidal solution of carbon nanostructures at dispersed phase concentration 0.01 mg/mL is stable for 1 month. Electron diffraction patterns and X-ray analysis of carbon nanostructures showed that nanostructure from brown coal is amorphous and nanostructure from anthracite is crystalline. Results of coal macromolecules modeling and graphene-like structures obtained from them are presented.     

Sorption charateristics of methane among various rank coals: impact of moisture

Enhanced coalbed methane (ECBM) in deep coal seams is being actively investigated around the world. Since the in situ coal seams are always saturated with water, methane sorption behavior on coal in the presence of water can help accurately assess the amount of recoverable methane. Thus, methane sorption isotherms have been measured on a high-rank anthracite, a low-volatile bituminous, a middle-volatile bituminous and a high-volatile bituminous coal with the manometric technology at 30 °C under six different moisture contents. The Dubinin–Astakhov (D–A) equation was used to fit the experimental sorption isotherm data. In all cases, the moisturized coals exhibited lower sorption capacity than the corresponding dry materials and moisture has a significant effect on CH₄ sorption capacity. The maximum sorption capacity, V ₀, displays a linear decline with the moisture content for the Changcun and Malan samples, but it is nonlinear for the other two coal samples. The net heat of CH₄ sorption, βE, is also reduced by the presence of water, but varies only slightly between a relatively small span of about 8.8 and 10.0 kJ mol^?1 for the dry samples studied, despite the difference in coal rank. In addition, the maximum sorption capacity of CH₄ in dry coals presents the typical “U-shape” trend with coal rank. Moisture has a greater impact on the sorption capacity in low-rank coals than that in high-rank coals. The mechanisms responsible for the effect of moisture on CH₄ sorption among various rank coals are also presented. The pore-blocking effect is the main influencing factor for high-rank anthracite, whereas, the competition sorption is dominant for low-rank coals.     

DSC-TG studies of coal structure modification by the inert gas helium

The influence of the inert gases helium and argon on the thermal properties of coal have been studied using DSC and TG. The coals studied were high-volatile bituminous coal and anthracite. It has been stated that the heat capacity of coal is strongly influenced by helium. This phenomenon is especially distinct for high-volatile bituminous coal. The authors attempt to explain this phenomenon.     

中国煤中溴的含量及分布

在测试分析中国27个省、直辖市和自治区的305个煤样中溴含量的基础上,从煤的不同成煤年代、不同变质程度以及不同聚煤区等方面分析和考查中国煤中溴的分布状况。结果表明,中国煤中溴的含量为0.12~69.66μg/g,因其对数值呈正态分布,故可用其几何平均值(7.04μg/g)表征中国煤中溴的含量,该值低于大多数其他国家煤中溴的平均含量,和日本煤中溴的平均值(7.10μg/g)较为接近。按煤中溴的平均值,中国13个省市小于5μg/g;9个省为5~15μg/g;5个省市高于15μg/g。根据煤的变质程度,中国煤中溴含量按照烟煤、无烟煤、褐煤、次烟煤顺序依次下降;根据成煤地质年代,按早石炭纪、新近纪、晚石炭纪、早二叠纪、中侏罗纪、晚三叠纪、早侏罗纪、晚侏罗纪、古近纪、中石炭纪依次下降;根据聚煤区,按西北、华北、华南、滇藏和东北聚煤区依次下降。中国煤中溴的分布受多种因素的影响,任何单一因素和其没有密切的相关性。     

Host phase of239,240Pu and241Am in deep-sea sediment

Host phases of fallout^239,240Pu and²⁴¹Am were studied in the surface sediments obtained in 1994 from abyssal basins of relatively small area of the western North Pacific. An analytical procedure involving sequential chemical extraction was employed for partitioning the host phases of the nuclides in sediment into five fractions: (1) exchangeable (2) bound to carbonate, (3) bound to hydrous Fe-Mn oxides, (4) bound to organic matter and (5) residual. Decrease of total^239,240Pu concentration with decreasing association of^239,240Pu with organic matter, high²⁴¹Am/^239,240Pu activity ratio in carbonate phase and somewhat high proportion of oxidized^239,240Pu in leachable phases suggest a possibility of post-depositional diagenetic remobilization of Pu from sediment to water column.     

用电子自旋共振谱研究我国一些煤的自由基

本文用电子自旋共振谱(ESR)研究了我国十种不同变质程度的煤。电子自旋共振最重要的参数是g值、自由基的浓度、线宽和线形。用这些参数与煤中的碳、氧等元素相关联,发现ESR参数与煤的变质程度有密切关系。