降雨主导型库岸滑坡变形时空分布特征

根据某大型水库近坝库岸滑坡8年的监测资料,对该滑坡变形的时空分布特征进行了分析。该滑坡变形的空间分布特征主要表现为3个方面的差异,即区域差异、高程差异和深度差异。而滑坡变形的时间分布特征主要体现在库水作用和降雨两个方面:在重点监测的Ⅱ区,库水作用只影响到其前端部分,对中、后部影响很小;该区的整体变形与降雨关系密切,响应明显。这些特征表明该滑坡为降雨主导型库岸滑坡,并有向稳定方向发展的趋势;但Ⅱ区特有的"后坐式"变形特征又存在一定的安全隐患,因此,该滑坡的监测还应长期进行。     

地震滑坡地形剖面线多重分形特征及其在稳定性判别中的应用

"5.12"汶川地震诱发了大量的滑坡和不稳定斜坡体,这些滑坡和不稳定斜坡体的稳定性影响到灾区社会经济发展和灾后重建。地震滑坡的不同稳定性状态孕育了滑坡地形剖面线的演化特征,并且地震滑坡地形剖面线直接地反映了在地震力作用下坡体的演变过程和演化机制。根据实测的汶川地震诱发的滑坡地形剖面线特征,研究了相对稳定滑坡、蠕滑阶段滑坡和不稳定斜坡的地形剖面线的分布特征,以及地震滑坡不同稳定状态下的地形剖面线的多重分形维数演化特征。研究结果表明相对稳定滑坡的多重分形维数演化特征的具有明显的有序性,处于蠕滑状态的滑坡和不稳定斜坡的多重分形维数演化出现明显的特征性拐点。     

中国碳排放强度与煤炭消耗的冲击效应分析

受能源消费结构的影响,煤炭作为我国经济发展的资源支柱,一方面推动着经济快速增长,另一方面也对中国节能减排、降低碳排放强度提出了挑战,因而准确认识碳排放强度与煤炭消耗之间的交互冲击作用机理,为挖掘碳减排路径提供了科学依据.本文选取1990 - 2008年间中国碳排放强度与煤炭消耗指标,采用EG协整检验证明碳排放强度与煤炭消耗之间存在长期稳定关系,并以此建立VAR模型和脉冲响应函数,考察碳排放强度与煤炭消耗之间的长期动态影响特征.冲击响应分析结果表明:(1)煤炭消耗比重的变化对碳排放强度的冲击影晌具有一定滞后性和波动性,但冲击作用长期持久;(2)碳排放强度对煤炭消耗比重的冲击影响在短期内较剧烈,但长期冲击影响不明显;(3)煤炭消耗比重的降低在长期内会促使碳排放强度的降低,因而可以通过降低煤炭消耗比重来达到降低碳排放强度的目的.最后,从结构性降低、产业传导性降低以及技术性降低等角度,提出减少煤炭消耗、降低碳排放强度的相关对策措施.     

滑坡泥石流的多源遥感提取方法

针对汶川地震灾区内滑坡泥石流多发的现象,分析了基于光学遥感数据和SAR数据的滑坡泥石流提取方法.光学遥感数据使用多期影像变化检测和灾后SAR数据使用特征提取的方法,可以分别有效地对滑坡泥石流信息进行提取.结果显示,文中使用的方法可为滑坡泥石流多源遥感监,测提供方法参考.     

Impact of initial and boundary conditions on preferential flow

Preferential flow in soil is approached by a water-content wave, WCW, that proceeds downward from the ground surface. WCWs were obtained from sprinkler experiments with infiltration rates varying from 5 to 40 mm h^− 1. TDR-probes and tensiometers measured volumetric water contents θ(z,t) at seven depths, and capillary heads, h(z,t) at six depths in a column of an undisturbed soil. The wave is characterized by the velocity of the wetting front, c_W, the amplitude, w_S, and the final water content, θ. We tested with uni-variate and bi-variate linear regressions the impacts of initial volumetric water contents, θ_ini, and input rates, q_S, on c_W, w_S and θ.The test showed that θ_ini influenced θ and w_S and q_S effected c_W. The expected proportionality of w_S ≈ qs^1/3 was weak and c_W ≈ qs^2/3 was strong.     

我国废铅蓄电池产生量与再生铅产能的讨论

废铅蓄电池是再生铅主要原料,铅蓄电池产量、进出口量、社会消费保有量,以及铅蓄电池消费使用领域与废铅蓄电池产生量有关。预测2015年废铅蓄电池产生量,并讨论我国再生铅产能规模,供再生铅产业结构调整与区域布局调整作参考。     

Numerical simulation of hydrogen–air detonation for damage assessment in realistic accident scenarios

An accidental hydrogen release within an equipment enclosure may result in the presence of detonable mixture in a confined environment. From a safety standpoint, it is then useful to assess the potential for damage. In that context, numerical simulation of the sequence of events subsequent to detonative ignition provides a useful tool, although with obvious limitations. This article describes the procedure, summarizes two case studies, and reviews the limitations. First, a hydrogen dispersion pattern is obtained from numerical simulation of dispersion, using a commercial package designed primarily for incompressible flow. This dispersion cloud is then used as the initial condition in an inviscid, compressible, reactive flow simulation. To force detonative ignition, a sufficiently large amount of energy is deposited in a small region that corresponds to the ignition location. Chemistry is modeled using a single step Arrhenius model. Because the wave thickness is small compared with the computational domain, a fine mesh is needed, limiting the practicality of the process to two-dimensional geometries. This is the most significant limitation; it is conservative. The two cases described in the paper include an electrolyzer, in which a small release occurs, leading potentially to some damage to the enclosure, and a reformer, in which the consequences are potentially more serious.     

滑坡动态变形过程的综合研究方法

影响滑坡变形破坏过程的因素具有复杂性和多变性,要合理评价和预测滑坡的动态发展过程,深入的地质原型调查是基础,地质分析不仅能为其它分析方法的正确使用提供资料,而且能直接对滑坡的变形破坏发展过程作出定性的判断。在此基础上建立力学模型,采用数学力学理论进行定量计算和反演分析,可进一步从本质上去把握滑坡变形破坏的发展规律。本文通过介绍李家峡水电站Ⅱ号滑坡的研究实践,说明了采用定性地质分析与定量力学计算相结合的研究方法揭示滑坡变形破坏动态过程的有效性。     

易贡巨型高速滑坡卫星遥感动态监测

多期卫星遥感数据与图像清晰地反映了易贡滑坡的演变及其地貌形态特征,通过专题对比解译与滑坡时程分析,重点监测和评价了滑坡堰塞湖溃决后汹涌水对下游两岸产生的重大生态破坏,结果显示,下游又新增了25个不同规模的浅层滑坡或滑落,新河床两侧新增的大面积滩地覆盖了两则的森林、草地;个别河段出现了移位改道。     

ANALYSIS OF WIND- AND SHIP-INDUCED SEDIMENT RESUSPENSION IN DULUTH-SUPERIOR HARBOR1

ABSTRACT: Suspended solids and ammonium concentration profiles measured at five locations in Duluth-Superior Harbor during July-October 1985 were analyzed to quantify wind and ship effects on sediment resuspension and resulting harbor water quality. Wind components from the SE quadrant correlated strongly with depth-averaged suspended solids concentrations that were unaffected by ship passage or thermal stratification. Winds from that quadrant have the largest fetch in the harbor. The highest correlation (r²= 0.93) was with the 6-hour average of the ESE wind velocity component. Multiple linear regression analysis of data from post-ship passage concentration profiles yielded numerical estimates of settling velocities of 0.08 to 0.25 cm s^?1, typical of ship-resuspended sediments, and vertical eddy diffusivities of 4 to 13 cm² s¹. The results suggest that ambient vertical eddy diffusivities in the harbor are less than 4 cm² s^?1 in the absence of ship passages and with winds less than 5 m s^?1 (10 knots).