Three-Dimensional Computations of Multiple Tandem Jets in Crossflow

1 .IntroductionAn effective method of wastewater disposal in estuarine and coastal watersisto discharge partiallytreated effluentthrougha submerged multiport diffuserlocated atthe end of a sea outfall .Atypical dif-fuser designinvolves multiple jets all discharginginthe same direction awayfromthe shoreline ,per-pendicular to an alongshore ambient current to minimize the environmental impact .This is one type ofa multiple jet groupin crossflow(MJGC) . Whenthe jets are arrangedintandem,withthe…     

涪陵页岩气田焦石坝地区含气量定量预测技术

页岩含气量是页岩气勘探选区和储层评价的一项重要指标。目前,利用地震资料对页岩含气性评价多停留在定性预测阶段,定量化表征方法尚不成熟。从已钻井的实测含气量出发,利用横波测井资料,分析实测含气量与地球物理参数之间的关系,利用数理统计学的思想,优选出密度、纵波阻抗、纵横波速度比、λρ 4个参数变量,建立了适合焦石坝页岩气田的含气量多元线性回归预测模型;通过叠前同时反演获得的密度、纵波阻抗等相关数据体,实现页岩含气量的定量预测,结果表明,预测的含气量与实钻结果吻合度较高,相对误差小,预测方法可靠;同时指出,焦石坝地区五峰组—龙马溪组一亚段含气量较高,为有利开发层段。     

炮集域压制海水鸣震的τ-p变换法

利用Radon变换压制多次波的传统做法一般都是先进行叠加速度分析,然后在CMP道集上做相应滤波处理.实际资料处理中,带有多次波的速度分析难以准确地提取速度,进而造成多次波压制的效果不够理想.有别于传统的做法,本文提出的方法通过对炮集记录进行同相轴重排,运用变换域自适应切除的τ-p变换(线性Radon变换)滤波,实现了直接在炮集记录中压制海水鸣震.实际资料处理表明,该方法对于海水鸣震多次波压制是一种行之有效的方法.     

声学地层剖面野外数据采集几个关键问题的解决

针对目前国内几款通用的声学地层剖面野外数据采集商业软件,分析探讨了国外软件在数据采集与存储中存在的几个关键缺陷,如GPS滞后、强能量反射同相轴相位与极性改变、深水数据采集存储等严重缺陷。为解决上述缺陷,作者以ChirpⅢ硬件系统为基础,分析国外商业软件缺陷产生的原因,并通过自主研发,提出了解决这些缺陷的方法。经野外实际工作测试,证实了文中所提方法的正确性与可靠性。     

南极普里兹湾沉积物中有机碳和总氮的含量与分布

利用中国多次南极科学考察获得的沉积物样品,对普里兹湾沉积物中有机碳(OC)、总氮(TN)的含量和分布以及OC/TN进行了分析。结果表明:普里兹湾表层沉积物中OC和TN的含量变化范围分别为0.14%~1.20%和0.02%~0.20%,平均值分别为0.63%和0.11%。OC/TN的变化范围为5.5~8.2,平均值为6.8。OC和TN含量呈现明显的正相关性,表明有机质来源相同,比值接近6.6,说明有机质主要为海洋生源沉积。两者平面分布趋势非常一致,且与沉积物中泥质含量呈显著正相关,湾内73°E以西区域OC和TN含量较低,而以东区域含量较高,这是上层水体生产过程和冰川携带陆源砂等因素共同作用的结果。垂直分布上,OC和TN含量总体上表层高于深层,OC含量随深度增加逐渐降低,达到一定深度后趋于稳定。较高的沉积速率加速OC的埋藏,5根柱样中OC的埋藏率为39%~91%,平均为66%,表明普里兹湾是重要的碳汇区。     

多水下机器人系统水动力计算的多线程实现

介绍多水下机器人(UUV)数字仿真平台的硬件结构以及单体UUV和多UUV系统的水动力计算流程,在此基础上利用Windows多线程技术实现多UUV的水动力计算,该方法已经用于多UUV数字仿真平台虚拟环境节点的设计中.系统仿真实验表明该方法设计的应用程序具有良好的执行效率和实时响应能力,为以后多UUV半物理仿真平台的水动力计算和实体多UUV系统水动力系数的验证奠定了基础.     

The low-mass classic Algol-type binary UU Leo revisited

New multi-color photometry of the eclipsing binary UU Leo, acquired from 2010 to 2013, was carried out by using the 60-cm and 85-cm telescopes at the Xinglong station, which is administered by National Astronomical Observatories, Chinese Academy of Sciences. With the updated Wilson-Devinney code, the photometric solution was derived from BVR light curves. The results imply that UU Leo is a semi-detached Algol-type binary, with a mass ratio of q = 0.100（±0.002）. The change in orbital period was reanalyzed based on all available eclipsing times. The 0 - C curve could be described by an upward parabola superimposed on a quasi-sinusoidal curve. The period and semi-amplitudes are Pmod = 54.5（±1.1） yr and A = 0.0273d（±0.0015d）, which may be attributed to the light-time effect via the presence of an invisible third body. The long-term period increases at a rate of dR/dr=＋4.64（±0.14）×10^-7d yr^-1, which may be interpreted by the conserved mass being transferred from the secondary to the primary. With mass being transferred, the low-mass Algol-type binary UU Leo may evolve into a binary system with a main sequence star and a helium white dwarf.     

Precambrian amphibolites and basic granulites of the south coast of Western Australia

Field relations and chemical variation trends suggest that amphibolite and basic granulite bands occurring throughout the Precambrian gneissic terrain of the south coast of Western Australia were derived from basic igneous rocks. It is not known whether the original rocks were mainly intrusive, extrusive, or pyroclastic, but occasional discordant contacts indicate that intrusive types are certainly represented.

The chemical affinities of the original magmas are not entirely clear. Present compositions suggest dominantly subalkaline affinities, although a significant proportion of the analised samples show some alkaline characteristics. Data for supposedly immobile elements (Ti, P, Zr, Nb, Y) show possible similarities to recent island‐arc and ocean‐floor basalts, but these are not sufficiently strong to permit any firm conclusions regarding the original tectonic environment of eruption or intrusion. This absence of clear chemical similarities of the amphibolites and basic granulites to basalts of any particular modern tectonic environment may suggest chemical modification during possible low‐temperature alteration (e.g. ocean‐floor or burial meta‐morphism) or subsequent high‐grade regional metamorphism and anatexis, or the inapplicability of currently recognised tectonomagmatic principles to the Precambrian.     

Predictive mapping of soil total nitrogen at a regional scale: A comparison between geographically weighted regression and cokriging

Accurately mapping the spatial distribution of soil total nitrogen is important to precision agriculture and environmental management. Geostatistical methods have been frequently used for predictive mapping of soil properties. Recently, a local regression method, geographically weighted regression (GWR), got the attention of environmentalists as an alternative in spatial modeling of environmental attributes, due to its capability of incorporating various auxiliary variables with spatially varied correlation coefficients. The objective of this study is to compare GWR and ordinary cokriging (OCK) in predictive mapping of soil total nitrogen (TN) using multiple environmental variables. 353 soil Samples within the surface horizon of 0–20 cm in a study area were collected, and their TN contents were measured for calibrating and validating the GWR and OCK interpolations. The environmental variables finally chosen as auxiliary data include elevation, land use types, and soil types. Results indicate that, although OCK is slightly better than GWR in global accuracy of soil TN prediction (the adjusted R² for GWR and OCK are 0.5746 and 0.6858, respectively), the soil TN map interpolated by GWR shows many details reflecting the spatial variations of major auxiliary variables while OCK smoothes out almost all local details. Geographically weighted regression could account for both the spatial trend and local variations, whilst OCK had difficulties to capture local variations. It is concluded that GWR is a more promising spatial interpolation method compared to OCK in predicting soil TN and potentially other soil properties, if a suitable set of auxiliary variables are available and selected.     

一类分数阶差分方程边值问题多重正解的存在性

研究一类带有分数阶边界条件的分数阶差分方程多重正解的存在性.分析该方程的Green函数的性质,引入上、下解的概念,并利用Guo-Krasnosel'skii不动点定理和上、下解的方法,分别建立该方程存在正解的充分条件,最后利用Legget-Williams不动点定理,讨论该方程多重正解的存在性.