海南岛干季化学风化产物输出及其控制因素

根据2014年1月实测的海南岛昌化江径流化学组成,运用物质平衡法和相关分析法估算化学径流组成的来源和控制因素,探讨流域化学风化产物HCO_3~-和溶解性硅(DSi)的输出及生态环境意义。结果表明昌化江流域水体呈中偏弱碱性,化学径流组成阴离子以HCO_3~-为主,阳离子以Ca~(2+)、Na~+为主。其中,77.30%的离子源于流域内硅酸盐岩的化学风化,1.38%的离子来源于碳酸盐岩风化,大气沉降对化学径流的贡献为5.45%,人类活动对干、支流化学径流的贡献分别为15.90%与21.04%,差异显著(P0.01)。地貌条件、岩性及径流深度是影响流域化学径流组成的关键因素。昌化江流域干季输入南海的HCO_3~-和DSi量分别为2.12×10~8 mol、1.38×10~8 mol,是南海海洋生态系统初级生产力的主要物质来源之一,在南海生态系统物质循环预算中不可忽视。     

潮滩湿地土壤有机碳储量及其与土壤理化因子的关系——以崇明东滩为例

基于上海崇明东滩2013年3月的实测数据,借助ArcGIS软件进行Kriging空间插值,运用SPSS 21.0软件进行相关分析及通径分析,研究了崇明东滩表层30 cm深度土壤有机碳含量以及环境因子的空间分布特征,并对土壤有机碳储量进行了估算.结果表明,崇明东滩表层30 cm深度土壤有机碳密度介于1.02～5.22kg· m-2之间,平均值为2.32 kg·m-2,土壤有机碳储量为1.15×10s kg.土壤有机碳含量、土壤全盐量、含水量和NDVI指数的空间分布规律类似,呈现北高南低、高潮滩高而低潮滩低的趋势.中值粒径和容重的空间分布规律类似,表现为北低南高,高潮滩小于低潮滩.高程和pH值的空间分布规律不明显,空间变异性较小.7项环境因子与土壤有机碳含量都存在显著相关性,其中土壤全盐量是影响崇明东滩表层土壤有机碳含量的最主要因子.     

The legacy of migration in response to climate stress: learning from the Gilbertese resettlement in the Solomon Islands

The long‐term threat of sea‐level rise to coral atoll and reef island communities in Kiribati, Tuvalu and other nations has raised the possibility of international migration. Historical resettlements in the Pacific may provide valuable insight into the long‐term effect of future climate change‐related migration on communities. This study evaluates the challenges faced by Gilbertese people resettled from modern‐day Kiribati to Ghizo in the Solomon Islands by the British colonial administration in the mid‐1900s. Drawing upon field interviews (n = 45) conducted in 2011 and the available historical literature, the study examines the circumstances of the initial failed resettlement in the equatorial Phoenix Islands, the subsequent relocation to Ghizo, and the recent concerns of the Gilbertese in Ghizo. Focus is placed on the struggle to recover from the 2007 tsunami that devastated the unprepared community. The analysis reveals that uncertainty about land tenure (raised by 61% of respondents) persists 60 years after resettlement, and is linked to the ability to recover from the tsunami, tensions with the Melanesian population, concerns over political representation, cultural decline, and education and employment opportunities. The Gilbertese experience can serve as a cautionary tale for policymakers considering mechanisms for facilitating climate change‐related migration.     

上海市崇明岛农业土壤中二噁英的现状研究及来源分析

为了解上海市崇明岛农用土壤中二噁英类化合物(PCDD/Fs)现状水平及其来源,于2021年6-7月采集上海市崇明岛31个农业土壤样品,采用同位素稀释法测定样品中17种2,3,7,8-PCDD/Fs的含量,并且对其现状水平、异构体特征以及来源进行初步分析。结果表明,31个土壤样品中均检出PCDD/Fs,质量分数为88.14~356.55 pg/g,对应毒性当量为0.64~2.20 pg I-TEQ/g,统计频率分析发现呈右侧拖尾的偏态分布,中位数为1.05 pg I-TEQ/g。经过比较,崇明岛农用土壤属于典型的背景土壤,土壤中二噁英类物质的污染属于较低水平。利用主成分分析(PCA)和正定矩阵因子分解法(PMF)对可能的来源进行分析,结果显示上海市崇明岛农业土壤中PCDD/Fs的主要来源为五氯酚(PCP)、水稻秸秆烟(RSS)和交通源(TS),占比分别为61.6%,23.2%和15.2%。结合采样地理位置推断,上海市崇明岛农业土壤中PCDD/Fs可能受到来自崇明岛自身农耕以及交通等因素的影响。     

横沙岛潮滩沉积物中重金属的空间分布与累积

长期以来,长江流域的工农业及城市生活排污一直没有得到有效的控制,这必将对下游河口地区的生态环境造成直接或潜在的威胁。因此,针对横沙岛目前的潮滩环境进行研究,并就潮滩质量和发展趋势进行评价非常必要。通过对横沙岛潮滩表层沉积物中重金属元素空间分布与累积的统计学分析,得知横沙岛潮滩环境总体比较清洁,但多年来受城市工业废水和生活污水排放,以及城市汽车尾气和工业粉尘干湿沉降的影响,局部地区表现出较严峻的污染形势,Cu、Zn、Cr、Pb的最高浓度分别达到背景值的2.34、4.24、2.74和1.63倍。通过对潮滩表层沉积物粒度和有机质含量的分析,指出水动力条件、潮滩生物活化作用是影响重金属空间分布和累积的主要因素。     

崇明东滩湿地沉积物砷的形态特征

于2008年4月在崇明东滩湿地开展野外调查,采集表层沉积物样品,参考Walter W W等提出的砷5步提取法进行总砷、砷的形态分析。结果表明:东滩湿地沉积物总砷含量5.33~19.74 mg/kg,各形态砷所占比例:弱交换态0.6%(0.5%~0.7%);强交换态5%(3%~7%);非晶形铁铝锰氧化物结合态28%(26%~29%);晶形铁铝锰氧化物结合态21%(19%~24%);残渣态46%(42%~51%)。     

2019年8月海南岛三亚地震的控震断裂及未来地震危险性分析

2019年8月20日,海南省三亚市天涯区连续发生两次有感地震.为研究本次地震的控震断裂及琼南地区未来的地震危险性,综合分析了琼南地区历史地震活动特征和主要断裂的构造活动特征.结果表明:近EW向九所-水断裂在琼南地区起主要控震作用,沿断裂带小型地震频繁而密集发生.震中周边的NW向乐东-田独断裂较其他方向断裂活动时代最新,...     

长春市热岛效应的时空演变研究

以长春市为例,借助1988年9月25日,1995年9月29日和2000年9月18日三个时相的TM/ETM+遥感影像,研究长春市近12年热岛效应的时空演化规律。研究发现:长春市热岛效应明显且多年稳定存在,热岛中心主要分布在宽城区南部、二道区北部伊通河两岸和绿园区西南部;绿园区西南部和宽城区西北部强热岛区面积呈逐年增加态势,二道区北部伊通河两岸热状况有所改善;从1998年到1995年和从1995年到2000年,热岛面积分别增加约9.32 km2和14.93km2,增长速度加快。     

海南岛西部非农用地土壤中的稀土元素地球化学特征

对海南岛西部发育典型的12个非农业土壤剖面REE的组成特征及其纵向变化规律进行研究发现,区内非农业土壤剖面不同层位之间的稀土元素具有一定的继承性,风化成土的基岩奠定了土壤中稀土元素的初始含量及土壤中呈现的LREE富集与Eu亏损的特点,而成土过程中稀土元素分异作用则进一步加剧土壤中LREE的富集和Eu亏损,土壤剖面浅部的氧化和水解作用致使Ce在浅层土壤中的富集,并导致由剖面深部至浅部,Ce呈现出正异常增大之趋势。区内稀土元素的赋存状态与稀土元素性质及其所处的土壤地球化学环境有密切联系,同一层中不同形态稀土元素含量总体上表现为残渣态>Fe-Mn结合态>有机态>可交换态(含水溶态)>碳酸盐态,而往土壤深部,残渣态所占比例逐步增大,Fe-Mn结合态、有机态与可交换态(含水溶态)所占比例逐步降低。     

The role of the Alliance of Small Island States (AOSIS) in the negotiation of the United Nations Framework Convention on Climate Change (UNFCCC)

The United Nations Framework Convention on Climate Change (UNFCCC), which was signed by some 153 countries at the Earth Summit in Rio de Janeiro, Brazil in 1992, represented a singular triumph for the geographically dispersed group of island states and low-lying coastal developing countries, located in the Pacific, Atlantic and Indian Oceans, as well as in the Caribbean, South China and Mediterranean Seas, and known as the Alliance of Small Island States (AOSIS). This article focuses on the goals of AOSIS during the negotiations leading up to the adoption of the UNFCCC. For the first time in the history of the United Nations, a group of small states, hitherto relegated to the sidelines, was able to develop a specific negotiating agenda addressing areas which are of overriding concern to them and succeeded in having those concerns incorporated in a legally binding Convention of historic importance. As this article reveals, AOSIS set itself 12 negotiating goals during the negotiating rounds leading up to the UNFCCC, and 10 of these 12 goals were realized. Nevertheless, AOSIS, whose member states are most vulnerable to the possible adverse effects of climate change, was particularly concerned about those provisions of the UNFCCC that were either watered-down significantly, made largely meaningless or excluded altogether. These include: the absence of definite targets or specific timetables for the significant reduction of carbon dioxide by the industrialized countries of the North; the lack of permanent and clear financing arrangements in particular the lack of definitive financial provisions for adaptive response measures to the adverse impacts of climate change such as sea-level rise; and the absence of a specific provision for the implementation of coastal zone management schemes for those countries most vulnerable to sea-level rise. As the UNFCCC moves into the implementation phase, AOSIS should and must build on its past success. To do so, it will need to develop clearly defined initiatives aimed at strengthening the commitments for financing and insurance, and to seek inclusion of a provision to develop and finance coastal zone management schemes for the most vulnerable small states. While the article covers the AOSIS negotiating period up to and including the Earth Summit in June 1992, we nevertheless postulate some possible objectives which the AOSIS group might wish to consider in what is sure to be an intensive post-Earth Summit phase of the UNFCCC, leading up to the first Conference of the Parties of that Convention.