从翡翠原石交易看翡翠市场的发展趋势

以翡翠原石投标为主体的缅甸珍宝玉石交易会（俗称“公盘”）一直是翡翠价格风向标,翡翠原石价格的上涨必然会推动成品价格的迅速跟进.通过对翡翠市场爆发式增长后的近几年原石交易特点的分析,发现所谓“原石价格上涨”完全是市场炒作的结果,一些玉商为了维护自身利益,聘请“枪手”投标,中标后又违约拒绝领标,造成原石投标交易现场火爆,价格屡创新高,但实际成交率却很低.从翡翠成品市场的反应来看,虽然价格有所上涨,但涨幅并不与媒体夸张的报道相适应.分析认为,玉商在翡翠原石交易中的行为需要进一步规范;在原石供应短缺和玉商极力维护自身利益的情况下,翡翠的价格不可能大幅度波动;高档翡翠因原料近于枯竭,价格还有进一步的上涨空间;在产能过剩的市场环境中,翡翠市场重归活跃尚待时日.     

深海海底边界层原位观测系统研发与应用

为进一步研究南海北部陆坡海洋动力过程对深海海底边界层的影响,研发了“深海海底边界层原位观测系统(In-situ Observation System for Bottom Boundary Layer in Abyssal Sea)”,ABBLOS。观测系统主体为坐底式深海运载平台,最大工作水深可达6 700 m(实际工作水深取决于搭载设备的耐压水深),是研究深海海底边界层问题的重要技术创新。观测平台由上下两部分框架结构组成,上部框架用于搭载和回收观测设备,下部支撑架为配重,并且用于提供距离海底1 m的观测空间;同时创新性地设计了“卡槽定位-螺栓紧固”的连接方式连接上下两部分,连接方式简单可靠,保证了平台回收成功率。ABBLOS集成了75 k-ADCP、高频ADCP、ADV、高精度压力计、海底摄像机等设备,以及甲烷、温盐深、浊度、溶解氧、氧化还原电位等传感器,首次实现了内波、中尺度涡等海洋动力过程与海底边界层物理化学参数的动态变化同步观测,特别是可以观测距离海底1 m高度范围的水体流速剖面,并且达到7 mm一层的垂向空间分辨率。研制完成后,2020年在南海北部陆坡神狐海域655 m和1 405 m水深处分别成功布放并回收,观测时间共计34天,采集到观测站位上覆海水的流速剖面结构,捕捉到了平均周期为1天1次的内波作用过程,以及海底边界层的多种物理化学参数。初步分析655 m水深处的观测数据后,发现深海海底边界层的温度、压力、溶解氧、密度和盐度等参数受控于海洋潮汐过程,尤其是温度和压力的变化基本与潮汐周期同步。海底边界层氧化环境较为稳定,甲烷浓度由高变低,但是基本在海洋溶解甲烷平均浓度范围内。与潮汐相比,内孤立波对深海海底边界层水体的影响程度较小,但是明显可以引起沉积物的再悬浮,引起的海底边界层的海水浊度从背景值的0.01 NTU增大到48 NTU,海底摄像机也记录到了内孤立波期间深海底层海水突然变浑浊的过程,说明南海内孤立波可以影响海底沉积物的输运。     

5000 m新型能源勘探智能钻探装备与技术研究

结合我国地下新型能源勘探工作的重大需求,开展了“5000 m新型能源勘探智能钻探装备与技术”的研究,取得了5000 m多功能交流变频电动钻机、多参数孔底自动监测装置、高温环保泥浆及泥浆性能自动测量装置、取心和无心钻进不提钻互换钻具等系列成果,填补了国内空白,推动了新型能源深部钻探技术向智能化方向发展。     

煤田地质超深孔钻探工艺

在对深部煤田地质钻孔钻进工艺研究的基础上,有针对性选择使用聚合物泥浆,解决了基浆配制用水及泥浆抗地表水水质污染问题。通过改变双管钻具长度和改换取心钻头的切削具,满足软硬互层对钻头钻进效率的影响。在煤系地层钻进中,除采用常规的单管钻具钻进外,在见煤预告下过后,采用加长双管取心钻具,既可保证了回次进尺,又可保证岩心的采取。多项措施落实,不仅解决了生产中的一些难题,收到了较好的效果,而且创造了河北省煤田地质局煤田地质单孔钻探深度2 009.12m的新纪录,为今后深部钻孔的施工积累了经验。     

应用描述词汇约简的OGC地理信息服务演绎推理

针对OGC地理信息服务在地理空间知识的有效组织和表达方面的能力比较弱,缺乏对服务信息的描述,数据丰富而知识缺乏,致使已有的数据在知识的表示和检索上存在缺陷,通过引入地理本体,按照基础地理信息要素分类,对地理信息服务的关键描述词汇进行提取,构建了地理信息服务本体库和实例数据库,应用粗糙集理论建立关键描述词汇约简模型,基于该模型实现了对地理信息服务实例数据库进行知识约简,形成最优实例数据库。最后应用地理信息服务本体库和实例数据库,基于演绎推理模型开发实例原型系统,实现了对地理信息服务对象的语义检索和推理,并通过试验从查全率和查准率两个指标验证了该方法的可行性、有效性和准确性。     

球近似艾黎-海斯卡宁均衡模型分析

针对传统的均衡重力异常方式基于平面近似,积分范围较小、计算公式的适用性受限、表征的信息量有限的问题,该文在球坐标下分析艾黎-海斯卡宁(Airy-Hesikanen)均衡模型。以计算点向径为半径,将地形分为布格球壳和粗糙地形两部分,计算其地形影响和均衡改正。在实验区,选用补偿深度21km、密度差0.678g/cm3的模型参数,采用该文公式和传统公式计算均衡重力异常,并比较分析其计算值。结果表明,以球近似Airy-Hesikanen均衡模型计算均衡重力异常值,在小积分范围以及平坦地区,与传统公式计算值的精度相当;但随着积分半径增加,球近似Airy-Hesikanen均衡模型计算值精度不断提高、变化更平缓,说明球近似AiryHesikanen均衡模型代替平面近似Airy-Hesikanen均衡模型应用于重力问题研究更为符合地球实际情况。     

基于反射地震资料探讨泥河湾盆地的新生代和中生代地层

查明泥河湾盆地新生界及中生界地层序列及基底的分布与赋存形态是研究泥河湾盆地形成机制的基础性工作。本研究在泥河湾盆地桑干河与壶流河交接处附近采集了四条测线的反射地震数据,通过对精细处理后的地震剖面进行详细分析,在剖面上厘定了三个具有明显强反射标志的地层,即古近系的玄武岩、侏罗系上统的含煤地层和侏罗系下统的含煤地层;其中,新近系沉积层与古近系玄武岩界面在地震剖面上出现的双程旅行时为0.3~0.6s,深度范围为300~500m,而第四系泥河湾组底界由南西到北东逐渐加深,其界面深度为200~300m;侏罗系上统含煤地层在地震剖面上出现的双程旅行时在0.8s上下波动,其深度约为1200m,探测出侏罗系上统顶界面的深度范围为800~1100m;侏罗系下统含煤地层在地震剖面上出现的双程旅行时为1.0~1.4s,深度范围为1800~2000m,由此推测出中生界侏罗系与古生界寒武系地层分界线的深度为2000m左右;根据地震反射波阻抗差别推测出新元古界和太古界地层的分界面在地震剖面上出现的时间约为2.5s,其深度为4000m左右。本研究通过四条反射地震测线的数据基本上查明了泥河湾盆地位于探测区处第四系泥河湾组底界面的深度分布范围及起伏形态、侏罗系上统顶界面和下统底界面的大致埋深,为查明泥河湾盆地新生界及中生界地层序列提供了基础性的参考信息。     

Stabilization of Bottom Hole Temperature With Finite Circulation Time and Fluid Flow

As an alternative to finite element or finite difference modelling, analytical solutions are derived by the method of Laplace transformation and numerical results obtained for several models of the bottom hole temperature stabilization. Included in the models are the finite circulation time, the thermal property contrast between the borehole mud and the surrounding formation, and the presence of radial or lateral fluid flow in the formation, all of which are found to have significant effects on the dissipation of the thermal disturbance induced by drilling.
The mud circulation is considered to have the effect of either maintaining the borehole mud at a constant temperature or supplying a constant amount of heat per unit length per unit time to the borehole. For small circulation times, the former reduces to the 'zero circulation' model in which the mud circulation creates an instantaneous temperature anomaly at the hole bottom; for small borehole radii, the latter reduces to the line source model and the traditional 'Homer plot'.
For typical drilling operations in which the bottom hole temperatures are measured several hours to several tens of hours after the hole is shut in, the new models generally predict higher equilibrium formation temperatures than does the Horner plot. However, predictions from the various models converge if the BHTs are taken after the hole has been shut in for a period which is greater than about five times the circulation period.     

Chlorinated hydrocarbons in the seawater and surface sediments of Blanca Bay,Argentina

In order to characterize our study area and to provide reference values to be used in the future to measure the changes produced by an increase in contamination, the concentrations of chlorinated hydrocarbons have been investigated in fifty-one samples of seawater, taken at four different depths: air-sea interface, surface, one metre and bottom waters, and in twenty-three samples of surface sediments from Blanca Bay, Argentina. Of eleven organochlorine compounds we were looking for (α BHC, lindane, heptachlor, δ BHC. aldrin, heptachlor epoxide, dieldrin, o-p′DDD, p-p′DDD, o-p′DDT and p-p′DDT), seven could be detected in seawater and three in surface sediments with the following mean concentrations: α-BHC=48·2 ng l^?1; lindane=54·2 ng l^?1; heptachlor=45·0 ng l^?1; δ BHC=12·5 ng l^?1; aldrin=61·8 ng l^?1 and ΣDDT=67·0 ng l^?1; and δ BHC=3·2 ng g^?1; lindane=4·2 ng g^?1 and heptachlor=1·0 ng g^?1 for seawater, regarding the surface waters, and sediment samples, respectively.Concentration factors among the different water layers were also studied to see if there was any correlation between chlorinated hydrocarbon contents and the water depths from which the samples were taken. As a mean value, the air-sea interface water contains 18 times more of these compounds than that of the water near the bottom. A comparison of the values corresponding to seawater and surface sediments from our study area with those levels measured in samples from other geographic locations is also presented.With the purpose to detect a relationship between chlorinated hydrocarbon concentrations and the contents of particulate matter (PM) on the one hand, and particulate organic material (POM) on the other hand, four groups of samples containing different amounts of PM and POM, respectively were formed. From a comparison of the results obtained, lindane, heptachlor and δ BHC showed a tendency to lower concentrations in those samples containing little PM whereas α BHC and aldrin remained without important changes. No significant correlation was found between organochlorine levels and contents of POM.