互花米草入侵盐沼湿地CH4和N2O排放日变化特征研究

甲烷（CH4）和氧化亚氮（N2O）是导致全球气候变暖的2种重要温室气体,探索其源汇及地域排放特征一直是全球变化研究领域的核心内容。CH4和N2O通量的日变化研究是正确估算大时间尺度下CH4和N2O排放量的基础。利用静态箱法原位观测了江苏沿海芦苇（Phragmites australis）、盐蒿（Suada salsa）、光滩、水面以及互花米草（Spartina alterniflora）入侵湿地CH4和N2O排放的日变化特征。结果表明,1）互花米草湿地地上部生物量为1.70 kg·m^-2,土壤有机碳质量分数为13.55 g·kg^-1;分别是芦苇和盐蒿湿地的2.50-3.43和2.15-4.15倍。2）互花米草和芦苇湿地土壤10 cm处氧化还原电位（Eh）有明显日变化,最低值出现在3：00,最高值出现在12：00;光滩和盐蒿湿地没有明显的日变化。3）互花米草湿地 CH4日平均排放通量为0.52 mg·m^-2·h^-1,是其他湿地的2.12-6.40倍;N2O日平均通量为-3.24μg·m^-2·h^-1,显著低于盐蒿湿地、光滩和水面（P＜0.05）。互花米草和芦苇湿地CH4排放通量最高值（0.73 mg·m^-2·h^-1和0.30 mg·m^-2·h^-1）出现在15：00,最低值（0.37 mg·m^-2·h^-1和0.17 mg·m^-2·h^-1）出现在3：00,均与土壤孔隙水中CH4浓度呈显著负相关（P＜0.05）。互花米草湿地CH4排放通量与10 cm土温、Eh和生态系统CO2净交换量（NEE）显著正相关（P＜0.05）。互花米草和芦苇湿地N2O通量9：00-18：00为负值,21：00—6：00为正值,均与NEE呈显著负相关（P＜0.05）。盐蒿湿地、光滩和水面CH4和N2O排放通量没有明显日变化特征。互花米草入侵提高了沿海湿地CH4排放,但降低了N2O排放,植物对CH4传输作用以及向根际传输O2和易分解有机物是导致互花米草和芦苇湿地CH4和N2O排放表现出日变化特征的原因。     

环境污染和生态破坏经济损失的估算模型

应用江苏省1988—2002年时序数据,建立环境污染与生态破坏经济损失的宏观估算模型,对影响环境污染与生态破坏的限制因子进行定量分析评价。     

Smoke alleviates adverse effects induced by stress on rice

Smoke and salinity are environmental hazards. Smoke produced DNA damage, inflammatory, and oxidative stress in humans while salinity reduced plant yield. However, smoke from plants is beneficial towards plant growth. In this study, smoke of two plants, Buhania varegata (1:1000 and 1:5000 dilutions (v/v)) and Cymbopogon jwarancusa (1:500 and 1:1000), were used to determine effects on different physiological and biochemical parameters in rice Basmati-385 (B-385) and Shaheen Basmati under different saline concentrations (control: 50, 100, and 150 mM). With increasing salinity, germination%, seedling growth, K⁺, Ca⁺, cell membrane stability, and total nitrogen and protein contents were decreased while Na⁺ content increased. However, seeds primed with different dilution of smoke significantly diminished the adverse effects of salinity and shown to produce positive responses in all of the above parameters. The most effective dilutions were 1:5000 for Buhania varegata and C-500 for Cymbopogon jwarancusa. It seems that priming with plant smoke solution is a potent stimulant for plant growth exerting a significant role in physiology and biochemistry of rice plants under saline condition.     

Biochemical speciation in chromium genotoxicity

The biochemical speciation of chromium compounds in mammalian cells is discussed with respect to uptake, metabolism, DNA binding and damaging. Whereas soluble hexavalent chromium is taken up rapidly and accumulated intracellularly after its reduction, compounds of trivalent chromium penetrate biomembranes about three orders of magnitude slower. Cr(VI) after its uptake is metabolised by electron donating compounds via Cr(V) to Cr(III) compounds. Chromium from various Cr(III) compounds, but not chromate, binds to chromatin in isolated cell nuclei. The DNA‐protein crosslinks and DNA strand breaks observed in rat liver and kidney after chromate administration are also found in vitro, when Cr(III) compounds (but not chromate) interacts with isolated nuclei. In the Chinese Hamster cell HGPRT mutation assay, three out of four tested Cr(III) complexes were found to be mutagenic. In a direct DNA strand break assay with supercoiled bacteriophage PM 2 DNA, neither chromate nor the four Cr(III) compounds tested caused nicks. However, the combined action of chromate plus glutathione as well as the isolated complex of pentavalent chromium, Na₄Cr(glutathione)₄, did cause DNA breaks. Reactive oxygen species are inferred to be the ultimate DNA nicking agents in this assay. In conclusion there appear to be two mechanisms of chromate genotoxicity; one with direct DNA damage caused by Cr(V) species and one via DNA‐protein crosslinks formed with Cr(III), the final reduction state of chromate.     

彗星实验检测渤海主要入海河流遗传毒性

利用彗星实验检测渤海区主要入海河流遗传毒性.以虾虎鱼为受试生物,暂养在河口水样中,染毒48h,取外周血细胞,运用彗星实验检测外周血细胞内DNA损伤程度,以尾相(TM)作为DNA损伤程度指标,并据此评估入海河流邻近海域遗传毒性风险.实验结果表明,入海河流中的特征污染物可导致虾虎鱼外周血细胞的DNA损伤,且损伤程度可以通过彗星实验定量分析,同时该试验方法操作简便、快速、灵敏度高,能够反映出多种污染因子的综合致毒能力.因此,通过彗星实验建立实验室检测入海河流遗传毒性方法具有可行行和创新性.     

土默川平原不同盐渍化土壤酶活性特征的研究

为探讨土默川平原不同盐渍化程度土壤酶活性的特征,选取轻度、中度、重度盐渍化土壤为对象,采用滴定法、比色法研究了0～40 cm土壤蔗糖酶、过氧化氢酶、脲酶、碱性磷酸酶4种酶活性不同季节的变化特征。结果表明:随盐渍化程度加剧,4种酶活性均呈现逐渐降低的趋势,蔗糖酶活性变化在0.65～36.55 mg·g-1、过氧化氢酶活性变化在2.76～3.35 mL·g-1、脲酶活性变化在0.003～0.018 mg·g-1、碱性磷酸酶活性变化在0.10～0.98 mg·g-1;土壤蔗糖酶、脲酶、碱性磷酸酶随土层加深酶活性降低,而过氧化氢酶活性表现为20～40 cm土层高于0～20 cm;不同盐渍化程度土壤酶活性的季节性变化趋势不同,过氧化氢酶和蔗糖酶活性的季节性变化呈先升高后下降的趋势,脲酶和碱性磷酸酶活性的季节性变化呈先升高后下降再升高再下降的趋势,碱性磷酸酶随时间的推移酶活性逐渐上升,且土壤酶活性出现峰值也不同,蔗糖酶和脲酶出现在8月,过氧化氢酶出现在7月,碱性磷酸酶出现在9月;不同盐渍化程度土壤酶活性在一个生长季内变化幅度表现为轻度>中度>重度盐渍化;不同盐渍化土壤碱性磷酸酶与脲酶、蔗糖酶活性呈极显著正相关,与过氧化氢酶活性呈极显著负相关,蔗糖酶与脲酶活性呈极显著正相关。因此,土默川平原不同盐渍化程度土壤酶活性及其季节性变化差异显著,土壤盐分含量影响着该地区土壤酶活性的变化。     

基于卸加载响应比的滑坡稳定状态评价与划分

为有效评价与预测滑坡的稳定状态,提出基于卸加载响应比参数的滑坡稳定状态划分的新方法.在阐述卸加载响应比理论内涵的基础上,从损伤力学角度探讨并建立了卸加载响应比与损伤变量的相互关系,并进一步通过分析滑坡稳定安全系数与损伤变量之间的相互关系,建立了卸加载响应比与滑坡稳定安全系数的定量关系.参照相关规范和标准,以卸加载响应比值划分了滑坡稳定状态区间.并以新滩滑坡为例,计算所得卸加载响应比所对应的滑坡稳定状态与实际情况相吻合.说明可以用卸加载响应比参数对滑坡稳定状态进行评价,它与滑坡稳定安全系数一样具有理论和实际应用价值.     

单元模态应变能法在输电铁塔损伤识别中的应用

输电塔结构在灾害中发生倒塌的现象时有发生,故而对输电塔结构进行健康监测具有重要的实际意义。介绍了单元模态应变损伤指数(EMSDI)在结构损伤识别中的表达式,并将其应用于输电铁塔模型试验中。采用单元形函数代替原有模态曲率计算方法,可有效降低计算单元模态应变能的计算误差,从而增加了识别的准确性。在输电铁塔仿真模拟和试验中,对该识别方法的准确性和可靠性进行了验证。实例表明:单元模态应变损伤指数法能够准确地识别出结构的损伤位置,并可在某种程度上反映出损伤程度,可以应用到实际输电塔结构损伤识别中。     

Normalized tornado damage in the United States: 1950–2011

In 2011, thunderstorms in the United States resulted in 550 deaths from tornadoes and more than $28 billion in property damage, according to data from the US National Oceanic and Atmospheric Administration, with the vast majority of economic losses resulting from tornadoes. This article normalizes U.S. tornado damage from 1950 to 2011, using several methods. A normalization provides an estimate of the damage that would occur if past events occurred under a common base year's societal conditions. We normalize for changes in inflation and wealth at the national level and changes in population, income and housing units at the county level. Under several methods, there has been a sharp decline in tornado damage. This decline corresponds with a decline in the reported frequency of the most intense (and thus most damaging) tornadoes since 1950. However, quantification of trends in tornado incidence is made difficult due to discontinuities in the reporting of events over time. The normalized damage results are suggestive that some part of this decline may reflect actual changes in tornado incidence, beyond changes in reporting practices. In historical context, 2011 stands out as one of the most damaging years of the past 61 years and provides an indication that maximum damage levels have the potential to increase should societal change lead to increasing exposure of wealth and property.