新乡市道路灰尘中PAHs的污染特征和来源解析

系统探讨了新乡市道路灰尘中PAHs的含量、分布,并解析了道路灰尘中PAHs的来源,并对新乡市道路灰尘中PAHs进行了生态风险评价,结果表明,新乡市道路灰尘中美国EPA优先监测的16种PAHs的检出率为100%,16种PAHs总量在42.1—8720 ng.g-1之间,平均含量为3223 ng.g-1.与国内外其它城市相比,新乡市道路灰尘中PAHs含量较低,与新乡市的经济发达状况呈现正相关.新乡市道路灰尘中PAHs的组成以4环PAHs为主,占PAHs总量的40.18%.通过多特征比值,对新乡市道路灰尘中PAHs来源进行定性判断,表明其主要来源于石油及其精炼产品的不完全燃烧和木柴、煤的燃烧;进一步通过因子分析/多元线性回归分析表明,新乡市道路灰尘中PAHs主要来源于汽油车、煤和木柴的燃烧以及柴油车的排放,其平均贡献率分别为33.5%、50.6%和15.9%.各种PAHs组分的单因子指数评价结果表明,新乡市道路灰尘已经受到PAHs的较严重的污染.所有样品的综合污染指数表明,新乡市道路中PAHs的综合污染指数的范围在0.09—9.95,平均值为3.38,充分表明新乡市道路灰尘已经受到严重的PAHs污染,具有较高的生态风险.     

238U、239Pu在板岩和土壤中迁移速度的实验模拟

以西南某低放废物处置库地质环境中板岩和土壤介质为研究对象,开展了238U和239Pu核素在这两种地质介质中的动态迁移实验研究,通过氚穿透实验(地下水流速=1 mL.min-1、实验柱连续淋洗时间=180 d)得到氚在板岩中的弥散系数DL为0.027 cm2.min-1,弥散度αL为0.324 cm,在土壤中的弥散系数DL为0.064 cm.2min-1,弥散度αL为0.895 cm.通过淋滤实验(地下水流速=0.1 mL.h-1、实验柱连续淋洗时间=350 min),得到了238U在板岩和土壤介质中的迁移速度分别为6.1—8.1 cm.a-1和7.3—8.5 cm.a-1,239Pu在板岩和土壤介质中的迁移速度分别为4.1—6.1 cm.a-1和3.7—4.9 cm.a-1.     

办公室地面灰尘中PAHs污染的时间变化规律及人体健康风险

为探究室内地面灰尘中15种多环芳烃(PAHs)污染的时间变化规律,于2012年3—7月对北京市一座办公楼内的某办公室进行了每周一次的连续高密度灰尘样品采集。利用高效液相色谱-荧光检测器检测15种PAHs含量。结果表明,该办公室内灰尘样品中∑PAHs浓度范围为1 180~24 300 ng·g~(-1),平均浓度为8 960 ng·g~(-1)。总体上,检出的PAHs以3环PAHs为主,其中菲占PAHs总量的59%以上,其次是4环和5环PAHs,4环PAHs中占的比重最高,约占4环PAHs总量的34%。该办公室内灰尘中∑PAHs的浓度存在显著的时间变化差异,总体表现为∑PAHs浓度随气温升高而降低的趋势。源解析结果显示,机动车排放源、石油源、木材与煤燃烧是北京市室内灰尘中PAHs的主要来源。健康风险评估结果显示,ILCR皮肤接触ILCR手口摄入,且CR均值大于10-6,说明该采样点的PAHs污染存在"潜在致癌风险"。     

低剂量丙烯酰胺多世代持续暴露对秀丽隐杆线虫的损伤作用

论文研究了丙烯酰胺(acrylamide,AA)低剂量多代持续暴露对模式生物秀丽隐杆线虫(Caenorhabditis elegans,C.elegans)的发育、生殖、寿命和捕食行为能力的影响。将线虫暴露于不同剂量水平的AA中,检测对当代线虫的发育周期、后代数量、寿命和捕食行为的影响,结果显示,1.0 mmol·L~(-1)AA水平可诱发当代线虫发育周期延长和后代数量减少(P 0.05),0.05mmol·L~(-1)和0.001 mmol·L~(-1)水平可分别诱发捕食行为能力下降和寿命缩短(P0.05)。进一步选取对当代线虫不产生明显损伤效应的AA剂量,将线虫进行多代持续暴露处理,结果显示,0.01 mmol·L~(-1)AA分别可在第2代g1和第3代g2诱发发育周期延长和后代数量减少(P0.05),0.005 mmol·L~(-1)AA可在第2代g1引起摄食行为能力下降,0.0001 mmol·L~(-1)(约7μg·L~(-1),低于推测人的平均AA暴露水平)的AA在第2代g1即可诱发寿命缩短(P0.05)。以上结果表明AA生物学毒性可以在后代间积累,极低剂量AA多代持续暴露仍可诱发生物学损伤。     

辽宁省气候-植被指标时空变化特征及森林适宜性分析

基于辽宁省56个气象站的气象资料,利用Kira的温暖指数（WI）、寒冷指数（CI）和徐文铎的湿度指数（HI）分析辽宁省近40年（1967-2006年）气候-植被指标的时空变异。结果表明,就辽宁省区域平均值而言,WI指数呈升高趋势,每10年增加幅度为2.47℃·月,CI指数呈下降趋势,每10年下降幅度为2.31℃·月,HI总体呈下降趋势,波动较WI和CI明显,从气候—植被指数变化趋势看,对红松Pinus koraiensis Sieboldet Zuccarini、长白落叶松Larixolgensis等不利,而对油松Pinu stabulaeformis Carr、栓皮栎Quercus vari abilis Blume等树种有利。空间变化特征表现为,温暖指数界限呈向西北移动的趋势,表明暖温带落叶阔叶疏林带的适宜面积增加,而温带针阔叶混交林带的适宜面积减小;HI指数减小并且向东移,表明随着指数带的北移和东移缩小限制了原有针叶树种的生长,而对栎树Phytophthora ramorum等阔叶树种有利。     

Effect of soil crust on evaporation and dew deposition in Mu Us sandy land, China

The development of soil crust on sandy land may affect the surface hydrological process. This paper investigates the process of evaporation and dew deposition influenced by different soil surface types which were dominated by sand, primitive biotic crust, and advanced biotic crust, respectively, in the south fringe of Mu Us sandy land in Northwest China from July to September of 2006. The experimental results indicate that the advanced biotic crust could increase evaporation and dew deposition compared to the primitive biotic crust and bare sand although the differences between them were not significant. The average evaporation from advanced biotic crust, primitive biotic crust and sand was 6.8, 6.6, and 6.5 mm/d, respectively, and water content is around 16.2 % in the condition of initially identical soil. The average dew amount on advanced biotic crust was 0.116 mm/d with extreme 0.05 and 0.24 mm/d. The average values on primitive biotic crust and sand were 0.105 and 0.101 mm/d, respectively, with extreme 0.04 and 0.21 mm/d for both treatments. Also, the dew deposition on advanced biotic crust seemed stable and might rest for a longer time than that on primitive biotic crust and sand. The results suggest that the advanced biotic crust possibly facilitates evaporation and dew deposition. Therefore, the development of biotic crust may potentially enhance the hydrological circulation in the upper sand layer in sandy land.     

内蒙高腐殖酸地下水中碘的分布特征与IDD病的关系

为探讨碘在高腐植酸地下水中的分布特征 ,研究内蒙古河套平原地区 51份水样 .分析结果显示 ,水质偏碱 (平均值 pH=7.91 ) ,水中腐植酸和 COD含量均高 ,地下水类型属于 HCO₃-Na和 HCO₃-Cl- Na型 .在这种高还原型盐水环境中水碘平均浓度达到 430 μg/L,超过了水碘安全浓度范围的上限 ( 5～ 200μg/L) .相关分析结果显示 ,水碘浓度与其它因素的相关顺序是 :COD>荧光强度 >电导率 >HCO^-₃>Cl^->Na⁺>pH>As>井深 .当地地下水中碘的分布呈现出碘浓度随腐植酸含量和盐渍化程度增加而增加的趋势 .由于这些因素的综合作用 ,当地没有发生高碘型碘缺乏病 ( IDD)的大面积流行 .     

云南稻核心种质F2主要形态性状变异及地理生态研究

种质资源是水稻育种的重要基因来源.掌握育种材料遗传背景信息,可为发掘优异种质,选育优良性状新品种提供依据.以548份云南稻核心种和云南主栽籼稻品利慎屯502(Oryza satica)、粳稻品种合系35(Oryzasatica)配制的杂种F2(498份)为材料,采用群体遗传学的方法,研究云南稻核心种质杂种F2代的11个形态性状的综合变异系数、遗传多样性指数(Shannon指数)及其地理分布.结果表明:(1)F2存在明显的性状分化和遗传变异,以有效穗、穗颈长、穗下节长、每穗实粒数、秕粒数、总粒数和结实率的综合变异系数高,遗传多样性丰富;(2)滇西南(临沧、思茅、德宏、西双版纳)和滇东南(文山、红河)的材料在表型性状上存在更大的分化,综合变异系数高,遗传多样性丰富;保山、昭通、曲靖次之;怒江、丽江、迪庆、大理最低.     

Effect of soil crust on evaporation and dew deposition in Mu Us sandy land, China

The development of soil crust on sandy land may affect the surface hydrological process. This paper investigates the process of evaporation and dew deposition influenced by different soil surface types which were dominated by sand, primitive biotic crust, and advanced biotic crust, respectively, in the south fringe of Mu Us sandy land in Northwest China from July to September of 2006. The experimental results indicate that the advanced biotic crust could increase evaporation and dew deposition compared to the primitive biotic crust and bare sand although the differences between them were not significant. The average evaporation from advanced biotic crust, primitive biotic crust and sand was 6.8, 6.6, and 6.5 mm/d, respectively, and water content is around 16.2 % in the condition of initially identical soil. The average dew amount on advanced biotic crust was 0.116 mm/d with extreme 0.05 and 0.24 mm/d. The average values on primitive biotic crust and sand were 0.105 and 0.101 mm/d, respectively, with extreme 0.04 and 0.21 mm/d for both treatments. Also, the dew deposition on advanced biotic crust seemed stable and might rest for a longer time than that on primitive biotic crust and sand. The results suggest that the advanced biotic crust possibly facilitates evaporation and dew deposition. Therefore, the development of biotic crust may potentially enhance the hydrological circulation in the upper sand layer in sandy land.     

云南粳稻核心种质杂种后代孕穗期耐冷性研究

以236份云南地方粳稻核心种质和云南主栽梗稻Oryza satica品种合系35配制的杂种F5、BC1F4、BC2F3和BC3F2为材料,在昆明自然低温平均17.8℃(冷害)条件下,对亲本及其后代进行孕穗期耐冷性研究.结果表明:①亲本耐冷性状间的相关性明显高于其杂种后代,不同世代间总体趋势为随着回交世代增加其性状间相关性减弱.在亲本及其杂种后代间耐冷指标性状穗颈长、穗下节长、每穗实粒数、每穗秕粒数与结实率均呈较高的(≥0.370)极显著(n=236,R0.01=0.181)相关.②株高、穗颈长、穗下节长等耐冷性状在亲本强弱耐冷系统群间的差异明显,表现为亲本耐冷性强的材料秆和穗较长、穗粒数较多,同一性状变异程度减小.但随着回交代数的增加,这些性状的平均值逐渐趋同于轮回亲本,差异减小.③穗颈长、穗下节长、每穗实粒数、每穗秕粒数与结实率在5个稻作区间的变化规律呈现一致性,亲本和F5的差异较大,而BC2F4、BC2F3和BC3F2的差异较小,且趋同于轮回亲本.通过连续回交,在BC3F1即可获得耐冷性状表现良好的材料.