空中战场复杂电磁环境分析

信息化条件下,空中战场呈现出电子设备密集、电磁环境复杂的特征。在复杂电磁环境下,各武器装备受到来自不同平台、不同形式的电磁威胁。这些电磁威胁造成了空中战场武器装备性能下降,指挥控制难度增大,整体作战能力降低。在分析空中战场电磁环境特点的基础上,对空中战场的电磁威胁环境进行了研究,还分析了复杂电磁环境对空中作战的影响。并从强化电磁环境意识和加强专业人才培养两个方面提出了应对策略。     

模拟沉积磷迁移转化行为的铁盐影响机制研究

室内模拟研究了沉积物中不同形态磷在不同浓度铁盐影响下,在沉积层中的垂直迁移转化行为.结果表明,分别向模拟系统投加的10 mL和50 mL的1 mol/L FeCl_3溶液,沉积层中磷的含量降低,投加30 mL的1 mol/L FeCl_3溶液时,沉积层中磷含量增加.沉积物中适当的铁盐会阻止沉积物磷向水体释放,铁盐浓度过高或过低,在一定程度上都会促进沉积物中磷的释放,实验结果对研究内源磷释放与湖泊富营养化有重要的意义.     

闽江河口芦苇潮汐湿地甲烷通量及主要影响因子

2007年利用静态箱-气相色谱仪法对闽江河口区最大的鳝鱼滩芦苇湿地和入侵种互花米草斑块涨潮前、涨落潮过程及落潮后甲烷通量季节动态进行了原位测定,并利用室内培养-气相色谱仪法测定了芦苇湿地不同土层土壤甲烷产生潜力.结果表明,鳝鱼滩芦苇湿地全年均属于大气甲烷的排放源,排放通量具有明显的季节变化;涨潮前、涨落潮过程和落潮后甲烷通量大小并无一致的规律,平均排放通量分别为5.13、5.06和4.74 mg·m-2·h-1,差异不显著,其中涨落潮过程排放到潮水和大气环境的甲烷通量分别为2.98和2.08 mg·m-2·h-1.互花米草入侵斑块年均甲烷排放通量(11.02mg·m-2·h-1)明显高于芦苇湿地年均甲烷排放通量(4.98mg·m-2·h-1),互花米草入侵明显增加了闽江河口区湿地的甲烷排放通量.芦苇湿地0～40 cm土壤中甲烷产生潜力范围为0.029～0.123μg·g-1·d-1,0～5 cm土层的甲烷产生潜力最大,且与其它土层差异显著(P<0.05).气温、土壤温度和地上生物量对芦苇湿地甲烷排放影响显著(P<0.05),落潮后芦苇湿地甲烷排放通量与盐度有负相关关系.     

Acid deposition critical loads modeling for the simulation of sulfur exceedanceand reduction in Guangdong, China

The current acid deposition critical loads in Guangdong, China were calculated using the PROFILE model with a 3 km × 3 km resolution. Calculations were carried out for critical loads of potential acidity, actual acidity, sulfur and nitrogen, with values in extents of 0–3.5, 0–14.0, 0–26.0 and 0–3.5 kmol/(hm2·year), respectively. These values were comparable to previously reported results and reflected the influences of vegetation and soil characteristics on the soil acid buffering capacity. Simulations of S...     

Combined fluorescence and electrochemical investigation on the bindinginteraction between organic acid and human serum albumin

Human serum albumin (HSA) is a plasma protein responsible for the binding and transport of fatty acids and a variety of exogenous chemicals such as drugs and environmental pollutants. Such binding plays a crucial role in determining the ADME (absorption, distribution, metabolism, and excretion) and bioavailability of the pollutants. We report investigation on the binding interaction between HSA and acetic acid (C2), octanoic acid (C8) and dodecanoic acid (C12) by the combination of site-specific fluorescent probe, tryptophan intrinsic fluorescence and tyrosine electrochemistry. Two fluorescent probes, dansylamide and dansyl-L-proline, were employed in the displacement measurement to study fatty acid interaction with the two drug-binding sites on HSA. Intrinsic fluorescence of tryptophan in HSA was monitored upon addition of the fatty acids into HSA. Electrocatalyzed response of the tyrosine residues in HSA by a redox mediator was used to investigate the binding interaction. Qualitatively, observations made by the three approaches are very similar. HSA did not show any change in either fluorescence or electrochemistry after mixing with C2, suggesting there is no significant interaction with the short-chain fatty acid. For C8, the measured signal dropped in a single-exponential fashion, indicative of independent and non-cooperative binding. The calculated association constant and binding ratio is 3.1×106 L/mol and 1 with drug binding Site I, 1.1×107 L/mol and 1 with Site II, and 7.0×104 L/mol and 4 with the tryptophan site. The measurement with C12 displayed multiple phases of fluorescence change, suggesting cooperativity and allosteric effect of C12 binding. These results correlate well with those obtained by the established methods, and validate the new approach as a viable tool to study the interactions of environmental pollutants with biological molecules.     

污泥干化过程中苯系物(BTEX)的释放及其致癌风险评价

在模拟污泥干化的条件下,研究了4种类型污水污泥苯系物(BTEX)的释放特征及其影响因素.结果表明,在50-300℃的干化温度范围内,4种污泥的BTEX释放总置在4.20～161.90μg·m-3之间;在温度高于150℃之后,各类污泥中的BTEX释放量大幅增加;而低于150℃的情况下,污泥中BTEX的释放量仅占总BTEX释放量的5.09%.不同温度下污泥的BTEX释放量与其在污泥中的含量之间存在显著的线性关系.不同类型的污泥其所释放的BTEX组分之间具有较大的差别,污泥中BTEX的含量决定其所释放的数量,而其释放强度则取决于干化温度.对污泥释放BTEX进行健康风险评价表明,各类污泥在150～300℃下所释放的苯对暴露人员存在一定的致癌风险,其中女性相对于男性致癌风险更高.控制污泥干化温度可以最大限度地减少BTEX释放,进而降低致癌风险.     

九龙江流域氮的源汇时空模式与机理初探

综合运用定位监测、野外试验、模型模拟与GIS技术等手段和方法,定量研究了南亚热带地区九龙江流域和五川小流域氮的大气沉降、河流输送(地表径流)、淋失、反硝化和氨挥发等输入输出(源汇)时空模式与机理.结果表明,九龙江流域氮源以化肥与饲料输入为主(占总输入125.6kg·hm-2的86%).氮汇以氨挥发和河流输送为主(占总输出72.9kg·hm-2的82%).氮输入后50%以上进入大气和水环境,14.5%通过河流输送至河口与近海.大气氮沉降通量为14.9kg·hm-2,其中干沉降占34%,湿沉降占66%,形成1:2的干湿沉降结构;源于化肥施用与畜禽养殖引起的强烈氨挥发,氮沉降集中在春夏两季(占全年80%),且以铵态氮为主(39%以上).氮的径流输出及河流输送受人为氮输入与水文条件的双重控制,2004年九龙江向厦门海域输送无机氮11.5kg·hm-2,其中90%发生在春夏秋季(同期流量占全年89%);五川小流域总氯径流输出负荷为67.1kg·hm-2,其中85%发生在施肥量大、降雨集中的春夏两季(作物生长期);基流与降雨径流分别贡献25%和75%.总氮淋失负荷为27.5kg·hm-2,占总输入的9%;pH<5的酸性土壤带正电荷导致氮淋失以铵态氮为主(约占40%).九龙江流域反硝化通量为7.7 kg.hm-2,而氮挥发高达42.1kg·hm-2,氨挥发主要来自化肥施用与畜禽养殖(分别贡献50%和39%).减少春夏时期肥料氮的输入(养分管理),有效截留雨季的降雨径流(水文控制)是该流域氮素管理的关键.