中国全新世气候变化研究进展

全新世气候变化研究是古气候研究的一个重点。中国全新世气候变化的研究也是全球变化研究中重要的一部分。大量的研究工作为恢复中国全新世气候做了重大贡献。中国地形地貌复杂 ,又处在具有复杂时空变率的东亚季风控制范围内 ,这使得不同的研究工作者在一些问题上存在意见分歧。比较统一的意见是 :中国全新世始于约 10 .5kaBP ;在约 9～ 8kaBP左右为一段降温期 ;7～ 4kaBP为一段温暖期 ,通常称之为全新世大暖期 ;大约 3kaBP左右开始降温 ,至近代才又升温 ;约 130 0aA .D .左右进入小冰期 ,到 185 0aA .D .左右结束 ,其间又有几次比较明显的温度振荡。 185 0aA .D .至今为温度的上升期。对于气候变动的驱动因素 ,不同的学者看法不一 ;从长时间尺度看 ,太阳辐射变化是气候变化的主要驱动力。     

A numerical method for spherical particle motion in turbulent flow with large Reynolds number

ＩｎｔｒｏｄｕｃｔｉｏｎＴｈｅｓｏｌｉｄ／ｆｌｕｉｄｔｗｏｐｈａｓｅｆｌｏｗｓａｒｅｏｆｔｅｎｅｎｃｏｕｎｔｅｒｅｄｉｎｍａｎｙｅｎｖｉｒｏｎｍｅｎｔａｌ，ｃｈｅｍｉｃａｌａｎｄｈｙｄｒａｕｌｉｃｅｎｇｉｎｅｅｒｉｎｇ，ｓｕｃｈａｓｓｅｄｉｍｅｎｔｔｒａｎｓｐｏｒｔａｔｉｏｎｉｎｒｉｖｅｒｓ，ｗａｓｔｅｗａｔｅｒｆｌｏｗｗｉｔｈｓｏｌｉｄｐａｒｔｉｃｌｅｓａｎｄｓｏｏｎ．Ｒｅｃｅｎｔｌｙ，ｃｏｎｓｉｄｅｒａｂｌｅｅｆｆｏｒｔｓｒｅｇａｒｄｉｎｇｎｕｍｅｒｉｃａｌｐｒｅｄｉｃｔｉｏｎｓｈａｖｅｂ…     

复配絮凝剂在餐饮废水中的应用研究

将聚丙烯酰胺 (PAM)和聚铁 (PFS)进行复配 ,分别以COD值和透光脉动值 (R)为技术指标 ,探讨了在处理餐饮废水过程中各种变化条件对絮凝效果的影响。结果表明 :PAM与PFS有一最佳复配比例 ,COD去除率达 90 %以上 ;在此絮凝剂条件下 ,投加方式、搅拌速度和浓度等对R值都有显著影响。     

Modeling Free-Surface Fluctuation Effects for Calculation of Turbulent Open-Channel Flows

A new method of introducing the free-surface effects in the calculation of turbulent open-channel flows using the amplitude of the free-surface fluctuation is proposed along with a modeling method of the equation for the free-surface fluctuation. It can be incorporated in two-equation models like k-or k-type models by introducing the damping factor to represent the interaction of the eddies with the fluctuating free-surface. Test calculations for fully developed flows and those over backward-facing step indicate good agreement with direct numerical simulation results as well as experimental results.     

Study on the investment value and investment opportunity of renewable energies under the carbon trading system

China has promised to start the national carbon trading system in 2017. In the carbon trading system, the renewable energy projects may obtain additional benefits through the Certified Carbon Emission Reduction (CCER) trade. As the carbon price fluctuates along with the market conditions, such fluctuation enables the renewable power projects to acquire the rights of an option, i.e. it may contain an even higher value due to the uncertainties in the future. While making an investment decision, the renewable power companies may choose to make the investment immediately, or postpone the investment and accumulate more information to increase the return of investment; and for immediate investments, the return must be sufficient to exceed the potential value of a waiting option. To study the investment in renewable power projects subject to the fluctuation of carbon price, this paper adopts the trinomial tree model of real options to estimate the net present value (NPV) and real option value (ROV) of three types of renewable power projects; according to the decision-making rules of real options to defer, all the three types of projects will exercise the option to postpone the investment decision. This thesis also calculates the benchmark prices of the three types of renewable projects at different times, in the two situations of having no government subsidy and having the government subsidy, so as to determine the investment opportunity of a project. The benchmark price decreases gradually along with the increase of government subsidy, indicating that the government subsidy will stimulate the investment in renewable projects. The benchmark price also increases gradually along with the lapse of time, indicating that the uncertainty will increase together with the time span and thus requires an even higher carbon price to determine the investment opportunity. This thesis also analyzes the sensitivity of factors affecting the investment in renewable projects and draws the conclusion that the fluctuation of carbon price is positively related with the benchmark price of renewable power projects, which indicates that the fluctuation of carbon price increases the option value of an investment but postpones the time of investment. As the China’s carbon trading system improves gradually, the carbon price will reach a stable status, thus stimulate the power companies to invest in the renewable projects.     

天然沸石中离子交换平衡的离子特异性研究

沸石在改良土壤和保护环境等方面有着广泛的应用,研究沸石离子交换中的特异性效应对更好地利用沸石有着重要意义.碱金属离子在天然斜发沸石中的交换平衡时的最大吸附量存在着明显的特异性效应;对于同价的碱金属离子,其交换吸附能力差异随着离子浓度的降低而增大.这种实验现象不能用库仑力、离子体积、水合作用、色散力、经典诱导力以及表面络合等相关理论进行完整解释.分析发现,根本原因来自离子因量子涨落而产生的极化与沸石颗粒表面电荷产生的强电场之间的相互作用,这种相互作用导致了离子间偶极矩差异随着表面电位的升高而增大,进而使离子-表面吸附能差异增大,并出现不同的交换吸附能力.由于沸石表面电荷密度较高,离子体积效应对其在双电层中的分布也起着比较重要的作用,导致碱金属离子在沸石表面的交换平衡结果在高表面电位(绝对值大于0.2 V)下才表现出较大选择性,与低电荷密度表面上的交换平衡结果存在一定差异.     

三峡库区典型消落带土壤及沉积物中溶解性有机质(DOM)的紫外-可见光谱特征

溶解性有机质(DOM)是陆地生态系统的重要组成部分,在环境地球化学中扮演着重要角色.在测定三峡库区典型消落带土壤及沉积物DOM的紫外-可见光谱基础上,通过特征参数及光谱模型来获取DOM的地化特征和信息.紫外-可见光谱特征参数表明土壤DOM的芳香性、疏水组分及腐殖化程度都明显低于上层沉积物,与高程和土地利用类型无关;而所选择的4种吸收光谱模型中以模型2为最优.同时,不同模型和不同拟合波段均对DOM光谱曲线斜率(S)有影响:S值随波长增加而减小;而不同波段S值相关性存在差异,表明各波段S值仅反映DOM部分信息,而非全部.此外,特征斜率之比(SR)反映出表层沉积物所受降解程度(光漂白或生物降解)小于土壤和往年沉积物,其芳香性更高,分子量更大,参与降解的反应活性也更大;这表明DOM越新鲜,其受到的光照和生物作用相对较小,降解潜力越大.     

三峡库区消落带3种植物淹水后汞的动态变化及其对水体的影响

被淹没的植物是水库甲基汞异常升高的来源之一.为探寻淹水条件下三峡水库消落带植物中汞的动态变化特征及其对水体的影响,通过室内模拟试验,研究淹水条件下稗草、狗牙根、玉米秸秆中汞含量变化及其向水体释汞情况.结果表明,3种植物总汞含量范围为9.21~12.07 ng·g-1,甲基汞占总汞的质量分数约为1%~2%.淹水后,植物总汞含量逐渐降低,其降幅为35.81%~55.96%;而上覆水溶解态汞(DHg)浓度迅速上升,增幅为103.23%~232.15%,说明植物腐烂分解会向水体释放汞.淹水环境为植物体组织内甲基化提供了充裕条件,导致植物残体甲基汞含量升高,为初始含量的3.04~6.63倍,而上覆水溶解态甲基汞(DMe Hg)浓度也显著升高,为初始浓度的14.84~16.05倍.淹水期间,上覆水中DMe Hg与溶解氧(DO)浓度表现为极显著负相关,与可溶性有机碳(DOC)浓度存在显著正相关.而在整个淹水过程中,上覆水DHg浓度变化量为植物总汞释放量的41.74%~47.01%,且各植物残体总汞含量与上覆水DHg浓度存在极显著负相关.     

利用紫外-可见吸收光谱估算三峡库区消落带水体、土壤和沉积物溶解性有机质(DOM)浓度

溶解性有机质(DOM)是陆地和水生生态系统的重要物质,有色溶解性有机质(CDOM)是可用光谱测定的DOM组分.基于2012年7月采集的土壤和沉积物样品以及2012年11月采集的水体样品,通过单波长、双波长、吸收光谱斜率(S值)和三波长模型建立CDOM与DOM浓度之间的关系.结果表明,4种模型中三波长模型效果最佳,水体数据模型的决定系数为0.788,土壤数据模型的决定系数为0.933,沉积物模型的决定系数为0.856.同时,利用2013年随机采集的32个土壤样品和36个水体样品对模型精度进行检验,结果表明,土壤DOM浓度的相对均方根误差(RRMSE)和平均相对误差(MRE)分别为16.5%和16.9%,水体分别为10.32%和9.06%,相比土壤DOM而言,三波长模型对水体DOM的预测精度更高.     

电压波动及其改善方法

通过分析电压波动产生的根源，论述了电压波动的不良影响，提出了改善电压波动的方法。