杭州西湖冬、春季水体光学特性比较

于2007年冬、春季对杭州西湖主要湖区的水下光合有效辐射进行了研究,主要从光学角度讨论西湖的水质状况及其影响因素. 选用美国LI-COR公司的水下光量子仪(LI-COR 192SA)分层测定光合有效辐射(PAR),同时测定透明度,叶绿素a,悬浮物(SS),总氮和总磷等理化因子. 通过对不同深度处水下辐照度进行指数回归得到光学衰减系数(K_d). 结果表明,西湖水质和水体光学条件冬季优于春季,ρ(叶绿素a)和ρ(SS)低,透明度和真光层深度高. 水下光合辐射的垂直分布呈指数衰减. 从总体上来看,K_d冬季小于春季,外西湖高于其他湖区,并且由南至北逐渐升高. 冬、春季K_d分别为0.49～2.25和0.59～3.45 m－1. K_d与ρ(叶绿素a)和ρ(SS)呈正相关.浮游植物和悬浮物是影响西湖水下光照的重要因素. 降低浮游植物和悬浮物含量是改善西湖水体光学条件的重要内容.      

一种室外声屏障过渡区域绕射衰减测量方法

提出了一种声屏障声影区与声亮区过渡区域的绕射衰减室外测量方法。方法采用5ms的正弦波作为测试信号,利用声波到达时间的差异有效地排除地面反射和有限长声屏障两侧绕射的影响,并通过背景噪声频谱分析选取测试声以及对接受信号FIR滤波以最大限度降低背景噪声的影响,同时考虑了气象条件变化导致的大气衰减修正。为进一步验证方法有效性,选取直立声屏障作为试验案例。结果表明,与室内全消声室试验结果、几何绕射理论结果接近,试验精度高。     

塔里木西南缘下地壳低速层的成因:斜长角闪岩的纵波速度和衰减的限制

在1 0GPa,室温～1200℃条件下,测量了新疆库地地区斜长角闪岩的纵波速度(Vp)和品质因子(Q值),得出在1 0GPa恒压下,Vp和Q值随温度和深度的变化关系。结果显示,Vp和Q值随温度的升高而下降,观察实验样品并结合Vp和Q值与熔体含量的关系,发现部分熔融是影响Vp和Q值变化的主要因素。依据实验结果,并结合区域上压力梯度和温度梯度资料计算了Vp和Q值随深度的变化。结果表明Vp和Q值先随深度的增加而缓慢增大,在32km左右开始突然减小,表明开始出现低速层。结合温度和熔体含量的关系得出,低速层的出现可能是部分熔融的结果。塔里木及周边地区的地震测深以及地震反演的结果也显示,在相同的温度和压力条件下,地壳内部32～44km的范围内存在低速层,同时高温高压的实验结果与阿拉木图地区的Vp值相当一致,可以推测塔里木西南缘下地壳的岩石成分中含有斜长角闪岩。     

利用多台首波Pn、直达波Pg走时确定地壳厚度及波速

本文通过对首波Pn、直达波Pg的走时的反演,推导出地壳厚度、震源深度、P波在地壳中、壳幔边界的传播速度之间的关系式,利用多台地震记录确定一个区域内这些参数的值,从而建立出该区域的地壳模型。     

均匀各向同性弹性介质中各类震源引起的地震波

运用均匀各向同性完全弹性的无限介质中震源激发地震波的理论公式模拟了给定点的 地震图,分析了地震波的各项特性。     

超声波降解有机磷农药乐果的实验研究

报道了用超声波降解模拟废水中低浓度乐果的试验。探讨了超声波辐射时间、外加H2O2、溶液中乐果的初始浓度、溶液温度等因素对乐果降解效果的影响。试验表明，辐射时间延长，降解率增加，辐射120min后降解率达97．5％；加入浓度为1．27mg／ml的H2O2即可明显提高乐果的降解率，H2O2的添加量达2．44mg／ml后，降解率增加趋缓；乐果溶液初始浓度由0．08mg／ml增加到1．6mg／ml，降解率由87．5％降低到55％；溶液温度控制在30℃以下对超声降解有利。     

Dendroremediation of trinitrotoluene (TNT) Part 2: Fate of radio-labelled TNT in trees

BACKGROUND, AIM AND SCOPE: Problems of long-term existence of the environmental contaminant 2,4,6-trinitrotoluene (TNT) and necessities for the use of trees ('dendroremediation') in sustainable phytoremediation strategies for TNT are described in the first part of this paper. Aims of the second part are estimation of [14C]-TNT uptake, localisation of TNT-derived radioactivity in mature tree tissues, and the determination of the degree of TNT-degradation during dendroremediation processes. METHODS: Four-year-old trees of hybrid willow (Salix spec., clone EW-20) and of Norway spruce (Picea abies) were cultivated in sand or ammunition plant soil (AP-soil) in wick supplied growth vessels. Trees were exposed to a single pulse application with water solved [U-14C]-TNT reaching a calculated initial concentration of 5.2 mg TNT per kg dry soil. Two months after application overall radioactivity and extractability of 14C were determined in sand/soil, roots, stem-wood, stem-bark, branches, leaves, needles, and Picea May sprouts. Root extracts were analysed by radio TLC. RESULTS: 60 days after [14C]-TNT application, recovered 14C is accumulated in roots (70% for sand variants, 34% for AP-soil variant). 15-28% of 14C remained in sand and 61% in AP-soil. 3.3 to 14.4% of 14C were located in aboveground tree portions. Above-ground distribution of 14C differed considerably between the angiosperm Salix and the gymnosperm Picea. In Salix, nearly half of above-ground-14C was detected in bark-free wood, whereas in Picea older needles contained most of the above-ground-14C (54-69%). TNT was readily transformed in tree tissue. Approximately 80% of 14C was non-extractably bound in roots, stems, wood, and leaves or needles. Only quantitatively less important stem-bark of Salix and Picea and May shoots of Picea showed higher extraction yields (up to 56%). DISCUSSION: Pulse application of [14C]-TNT provided evidence for the first time that after TNT-exposure, in tree root extracts, no TNT and none of the known metabolites, mono-amino-dinitrotoluenes (ADNT), diaminonitrotoluenes (DANT), trinitrobenzene (TNB) and no dinitrotoluenes (DNTs) were present. Extractable portions of 14C were small and contained at least three unknown metabolites (or groups) for Salix. In Picea, four extractable metabolites (or groups) were detected, where only one metabolite (or group) seemed to be identical for Salix and Picea. All unknown extractables were of a very polar nature. CONCLUSIONS: Results of complete TNT-transformation in trees explain some of our previous findings with 'cold analytics', where no TNT and no ADNT-metabolites could be found in tissues of TNT-exposed Salix and Populus clones. It is concluded that 'cold' tissue analysis of tree organs is not suited for quantitative success control of phytoremediation in situ. RECOMMENDATIONS AND OUTLOOK: Both short rotation Salicaceae trees and conifer forests possess a dendroremediation potential for TNT polluted soils. The degradation capacity and the large biomass of adult forest trees with their woody compartments of roots and stems may be utilized for detoxification of soil xenobiotics.     

Inverse modeling of BTEX dissolution and biodegradation at the Bemidji, MN crude-oil spill site

The U.S. Geological Survey (USGS) solute transport and biodegradation code BIOMOC was used in conjunction with the USGS universal inverse modeling code UCODE to quantify field-scale hydrocarbon dissolution and biodegradation at the USGS Toxic Substances Hydrology Program crude-oil spill research site located near Bemidji, MN. This inverse modeling effort used the extensive historical data compiled at the Bemidji site from 1986 to 1997 and incorporated a multicomponent transport and biodegradation model. Inverse modeling was successful when coupled transport and degradation processes were incorporated into the model and a single dissolution rate coefficient was used for all BTEX components. Assuming a stationary oil body, we simulated benzene, toluene, ethylbenzene, m,p-xylene, and o-xylene (BTEX) concentrations in the oil and ground water, respectively, as well as dissolved oxygen. Dissolution from the oil phase and aerobic and anaerobic degradation processes were represented. The parameters estimated were the recharge rate, hydraulic conductivity, dissolution rate coefficient, individual first-order BTEX anaerobic degradation rates, and transverse dispersivity. Results were similar for simulations obtained using several alternative conceptual models of the hydrologic system and biodegradation processes. The dissolved BTEX concentration data were not sufficient to discriminate between these conceptual models. The calibrated simulations reproduced the general large-scale evolution of the plume, but did not reproduce the observed small-scale spatial and temporal variability in concentrations. The estimated anaerobic biodegradation rates for toluene and o-xylene were greater than the dissolution rate coefficient. However, the estimated anaerobic biodegradation rates for benzene, ethylbenzene, and m,p-xylene were less than the dissolution rate coefficient. The calibrated model was used to determine the BTEX mass balance in the oil body and groundwater plume. Dissolution from the oil body was greatest for compounds with large effective solubilities (benzene) and with large degradation rates (toluene and o-xylene). Anaerobic degradation removed 77% of the BTEX that dissolved into the water phase and aerobic degradation removed 17%. Although goodness-of-fit measures for the alternative conceptual models were not significantly different, predictions made with the models were quite variable.     

高层建筑承受纵向地震波时的安全核算构想

高层建筑可预期的灾变非至一端，这里仅探讨高层建筑的抗震性能问题。地震过程中楼体受到的是地震波和自身固有频率的共同作用，此时楼体是一个多维动态系统，其应力状态比传统方法所描述的力学模型要复杂行多。本文应用ANSYS三维仿真有限元软件，采用单点响应谱的方法，对楼体在纵向地震波作用下的应力状态和变形情况进行了分析。对楼体构件单元型式的选择、网格密度的确定、有限元模型的建立等也提出了自己的见解。在后处理中，用列表和图形的方式显示了楼体的位移和应用状态。     

极谱催化波法测定痕量亚硝酸根的研究

在含稀硫氰酸盐的底液中 ,在单扫示波极谱仪上 ,有一灵敏的亚硝酸根催化波。峰电位为 -0 .47V( vs·SCE)。阳极化二阶导数峰高与亚硝酸根浓度在 1× 10 - 7～ 5× 10 - 5mol/L 之间成线性关系。检测限达 5× 10 - 5mol/L( 2 .3ppbNO - 2 )。试验了多种共存离子对测定的影响 ,表明该法具有较好的选择性 ,尤其是大量硝酸根不干扰。应用该法测定了许多样品中的亚硝酸根 ,并对该波的机理进行了研究 ,结果证明该波是 [SCN· NO]催化溶液中的溶解氧还原所致