1991／1992年世界气象灾害评述

1991/1992年是厄尔尼诺年,也是全球自然灾害频发、重灾事件突出的异常年份。本文对发生在1991/1992年厄尔尼诺事件期间的全球主要气象灾害进行简介和评述。     

用几种溶样方法对典型土样中Pb、Cr、Ni、Cd、Mn、Cu、Zn的溶出情况比较

本文采用HNO_3、HCl-HNO_3、HNO_3-H_2SO_4-HClO_4,溶洋方法消解土样,用原子吸收法测定题述中的元素,并与HCl-HNO_3-HF-HClO_4全消解方法进行了比较.发现除用HF以外的其它酸溶法Pb、Cr的溶出较少溶出比分别低于55％和67％,主要原因是Pb、Cr包藏在土壤的矿物晶格中。     

Effect of Heavy Metals on the Blood Protein Biochemistry of the Fish CYPRINUS CARPIO AND ITS USE AS A BIO-INDICATOR OF POLLUTION STRESS

Cyprinus carpio were exposed to two non-essential (Hg and Pb)and two essential (Cu and Ni) heavy metal salts at lethal andsub-lethal concentrations. Blood serum total protein, serum globulinand serum albumin was analysed every 2 hr for 24 hrs andagain at 48 and 72 hrs. Serum protein and globulin level showedan intial sharp increase from 2 to 20 hrs, followed by decline thatextend over a period of 72 hrs. Serum albumin showed an initialimmediate decline from 2 to 4 hrs, followed by an intermittent period of recovery and decline that extend over a period of 72hrs. Both lethal and sub-lethal concentrations of metal salts elicited asimilar pattern of response varying only in magnitude. The use offish blood serum protein, albumin and globulin measurements as general indicators of pollutant stress response isdiscussed.     

ENSO与云南蒋家沟泥石流灾害发生的关系

通过分析近40年来出现的ENSO事件对云南东川蒋家沟泥石流活动的影响可知,El Ni(~n)o与LaNi(~n)a对其的影响正好相反,且El Ni(~n)o的影响大于La Ni(~n)a的影响.El Ni(~n)o年,泥石流年发生频次、径流量和输沙量偏少的概率均较大,泥石流活动减弱的倾向明显;La Ni(~n)a年,虽有一定的对应关系,但不如El Ni(~n)o年明显,且影响更复杂一些,总的来说,泥石流年发生频次、径流量和输沙量偏多或持平的概率较大.     

气候异常与中国小麦白粉病灾害流行关系的研究

分析了厄尔尼诺事件与我国冬小麦白粉病发病面积的相关关系。结果表明：在厄尔尼诺出现的起始年，冬小麦白粉病发病面积相对较小；在厄尔诺起始年至下一个厄尔诺起始年前的前一年，冬小麦白粉病发病面积趋势逐年增大，并在下一个厄尔尼诺起始年前一年达到最大值；在连续出现厄尔尼诺的年份，冬小麦白粉病发生面积逐年降低。厄尔尼诺事件通过引发主要麦区的诱水、温度异常来影响小麦白粉病的流行程度。造成厄尔尼诺年我国小麦白粉病发病面向相对较低的原因，与厄尔尼诺起始年前的冬半年寒潮活动加强造成冬小麦冻害严重，大大降低了小麦白粉菌的越冬基数及春季干旱不利于小麦白粉菌的侵染有关。     

Climate change and changes in global precipitation patterns: what do we know?

The objective of this paper is to synthesize the large literature recording changing patterns of precipitation in the observed data, thus indicating that climate change is already a reality. Such a synthesis is required not only for environmental researchers but also for policy makers. The key question is the broad picture at major regional and continental levels. Some interesting conclusions for this survey are emerging. For example, the review shows increased variance of precipitation everywhere. Consistent with this finding, we observe that wet areas become wetter, and dry and arid areas become more so. In addition, the following general changing pattern is emerging: (a) increased precipitation in high latitudes (Northern Hemisphere); (b) reductions in precipitation in China, Australia and the Small Island States in the Pacific; and (c) increased variance in equatorial regions. The changes in the major ocean currents also appear to be affecting precipitation patterns. For example, increased intensity and frequency of El Ni?o and ENSO seem associated with evidence of an observed "dipole" pattern affecting Africa and Asia, although this time series is too short so far. But the changing pattern calls for renewed efforts at adaptation to climate change, as the changing precipitation pattern will also affect the regional availability of food supply.     

FORECASTING DRY SEASON STREAMFLOW ON THE PEACE RIVER AT ARCADIA,FLORIDA, USA1

ABSTRACT: The Peace River at Arcadia, Florida, is a municipal water supply supplement for southwestern Florida. Consequently, probabilities of encountering low flows during the dry season are of critical importance. Since the association between Pacific Ocean sea surface temperatures (SSTs) and seasonal streamflow variability in the southeastern United States is well documented, it is reasonable to generate forecasts based on this information. Here, employing historic records of minimum, mean, and maximum flows during winter (JFM) and spring (AMJ), upper and lower terciles define “above normal,”“normal,” and “below normal” levels of each variable. A probability distribution model describes the likelihood of these seasonal variables conditioned upon Pacific SSTs from the previous summer (JAS). Model calibration is based upon 40 (of 50) years of record employing stratified random sampling to ensure equal representation from each decade. The model is validated against the remaining 10 samples and the process repeated 100 times. Each conditional probability distribution yields varying probabilities of observing flow variables within defined categories. Generally, a warm (cold) Pacific is associated with higher (lower) flows. To test model skill, the forecast is constrained to be the most probable category in each calibration year, with significance tested by chi‐square frequency tables. For all variables, the tables indicate high levels of association between forecast and observed terciles and forecast skill, particularly during winter. During spring the pattern is less clear, possibly due to the variable starting date of the summer rainy season. This simple technique suggests that Pacific SSTs provide a good forecast of low flows.     

Phytoremediation of Nickel-Contaminated Soils by Brassica Species

Two Brassica species Brassica juncea and Brassica carinata of the Indian mustard, were grown in an artificially Ni-contaminated soil to study the tolerance and Ni accumulation. Chelating agent, EDTA was applied at the rosette stage for enhancing the metal uptake. Nickel concentration over almost double that in control was observed in both the species with Ni contamination along with EDTA application. Specie B. juncea appeared to be slightly more tolerant and higher accumulator of Ni. In agreement with the earlier reports, the translocation of the pollutant metal to the shoot from the root seemed to be restricted in both of Brassica species at higher rate of Ni application plus EDTA. The results of the present study indicated that B. juncea has the potential to be hyperaccumulator of Ni.     

重金属Cr(Ⅵ)和Ni对旱伞草富集能力及其生理生化指标的影响

采用水培方法,研究了在不同重金属Cr(Ⅵ)(0~50 mg/L)和Ni(0~50 mg/L)浓度下旱伞草(Cyperus alternifolius)的富集能力及生理生化指标的变化规律。研究结果表明:(1)旱伞草中积累的重金属含量随处理浓度的增加逐渐增加,Cr(Ⅵ)在其地上部和根部富集量分别达到958.00 mg/kg和2 874.44 mg/kg,Ni在其地上部和根部富集量分别达到1 655.46 mg/kg和2 511.20 mg/kg;(2)在Cr(Ⅵ)和Ni胁迫下,随着Cr(Ⅵ)和Ni浓度的增加,旱伞草生物量、叶绿素含量、根系活力均呈先上升后下降的趋势;(3)脯氨酸的含量随着Cr(Ⅵ)胁迫浓度的增加,呈现为先上升后降低的趋势,而随着Ni胁迫浓度的增加,则为先缓慢上升而后急剧升高。旱伞草对Cr(Ⅵ)和Ni具有较强的富集能力且主要分布在根部,虽不是Cr(Ⅵ)和Ni超积累植物,但具有较强的稳定化能力,在污染水体的修复方面有一定应用潜力。     

生物炭和草酸活化磷矿粉对镉镍复合污染土壤的应用效果

采用室内培养实验,利用生物炭和草酸活化磷矿粉对镉镍复合污染土壤进行修复,比较两者不同配比对土壤重金属镉镍的修复效果及对土壤无机氮和微生物量氮(MBN)转化的影响.结果表明,随着草酸活化磷矿粉和生物炭施用量的增加,土壤p H逐渐增加,镉和镍均由弱酸提取态逐渐向可还原态、可氧化态和残渣态转化,生物有效性降低.其中,C50P3(50 g·kg~(-1)生物炭与3 g·kg~(-1)草酸活化磷矿粉)配施的修复效果最好,弱酸提取态Ni占全量的质量分数降低了37.0%,残渣态Ni增加了14.8%,弱酸提取态Cd含量占全量的质量分数降低了40.2%,残渣态增加了35.2%.施用修复剂40 d后,相较于C0P0(空白对照)处理,C50P0(单施50 g·kg~(-1)生物炭)处理与C0P3(单施3 g·kg~(-1)草酸活化磷矿粉)处理微生物量氮含量均分别增加了1.5倍和1倍;铵态氮含量分别减少了12.5%和6.4%,硝态氮含量分别降低了11.6%和10.2%.综合比较可知,生物炭和草酸活化磷矿粉配施对土壤重金属镉镍复合污染的修复效果要优于单施,且50 g·kg~(-1)生物炭与3 g·kg~(-1)草酸活化磷矿粉(C50P3)配施的修复效果最好,修复剂的加入促进了土壤无机氮向有机氮的转化.