滇05井水位动态的震前短临异常     

刘国寿 《地震研究》1998,21(3):282-285

本文根据滇０５井的观测情况,研究该井水位变化速率。经多元回归分析,发现该井水位变化受固体潮汐的影响是主要的。继而采用彼氏滤波方法,排除固体潮汐的影响,结果发现：滇０５井在中强地震发生前,水位动态反映出明显的短临异常。  相似文献   

泥页岩的X射线衍射定向指数与理化性能及井壁稳定的关系   总被引：1，自引：0，他引：1  

沈守文  沈明道  梁大川  张国钊 《沉积学报》1998,(2)

首次提出了泥页岩Ｘ射线衍射定向指数的测定方法,探讨了定向指数与矿物成分,定向指数与泥页岩理化性能（密度、回收率、膨胀率、阳离子交换容量等）的关系。并在定向指数的基础上,提出了综合指数的概念,然后以定向指数和综合指数为主要依据,对坍塌地层泥页岩进行了分类。这对于钻井工程上研究井壁稳定的机理,预防井壁失稳,具有重要的理论意义和实用价值。  相似文献   

德国大陆科学钻探计划的测井成就   总被引：3，自引：2，他引：1  

王祝文  李舟波 《世界地质》1998,17(2):67-72

德国大陆科学钻探计划（ＫＴＢ）经过８年多的努力,钻探了先导孔（ＶＢ）和主孔（ＨＢ）两口举世瞩目的科学钻孔。地球物理测井技术在这个计划中起到了不忽视的作用,本文简要介绍了在德国大陆学科钻探计划（ＫＴＢ）实施过程中,地球物理测井所取得的主要成就。  相似文献   

Relationship of Water Chemistry to Serum ThyroidHormones in Captive Sharks with Goitres     

Gerald L. Crow  Marlin J. Atkinson  Benny Ron  Shannon Atkinson  Arleene D. K. Skillman  George T. F. Wong 《Aquatic Geochemistry》1998,4(3-4):469-480

Captive whitetip reef sharks, Triaenodon obesus,at Sea Life Park (SLP) Hawaii, Waimanalo, Hawaii develop goitre, whereas, T. obesus at the Waikiki Aquarium (WAQ), Honolulu,Hawaii do not develop goitre. To determine theeffects of natural concentrations of iodine on thereduction of goitre, two sharks from SLP with goitrewere placed in an enclosed coastal lagoon with naturalseawater. Using ultrasound measurements the twogoitres were initially 11.4 cm and 14.6 cm in depthand after 3 months decreased to 4.7 cm and 5.7 cm. Radioimmunoassay analysis of the thyroid hormoneT3 sera concentrations were initially 0.22 ng/mland 0.33 ng/ml and increased to 1.84 ng/ml after beingplaced in the lagoon. Sera T4 were initially0.93 ng/ml and 0.99 ng/ml and increased dramaticallyto 17 ng/ml and 56 ng/ml. Over the six month samplingperiod, two resident sharks in the lagoon with normalthyroids had sera T3 concentrations from 0.89ng/ml to 1.1 ng/ml, and sera T4 concentrationsfrom 3.1 ng/ml to 7.9 ng/ml. The hypothyroidcondition in the SLP goitred-sharks is likely linkedto the low environmental iodide (<0.005 M), andhigh nitrate (111 M) of SLP water. The WAQwell-water facility was characterized by anoxic waterwith high iodide (0.60 M), total iodine (1.90M), and typical nitrate (24.6 M)concentrations of interstitial groundwater. Thedifference of iodide concentration of SLP and WAQ tankwater (<0.005 M versus 0.60 M) wasdirectly related to the hydrogeology of the well-watersources. To avoid goitre in marine aquarium systems,we recommend maintaining iodide concentrations of atleast 0.15 M.  相似文献   

水平井降水技术在热力隧道暗挖工程中的应用   总被引：3，自引：0，他引：3  

叶发广  伍军 《水文地质工程地质》1998,25(3):53-54

在北京地区,我们首次成功地采用水平辐射井技术对双榆树热力隧道暗挖段进行地下降水。利用甲方的两处隧道工作竖井和另制作的一口大直径竖井,共施工水平孔３０眼,总长度达１５００ｍ,降水控制条带状隧道长度为３１０ｍ。开挖证实,降水效果显著,在地面以下降低地下水位的该项技术取得了明显的社会和经济效益。  相似文献   

SLUG试井污染检测乘积图版及其应用   总被引：2，自引：2，他引：0  

冯文光 《矿物岩石》1998,18(4):79-85

本研究获得了ＳＬＵＧ试井解与定产量试井解的数学关系式并制作出ＳＬＵＧ试井乘积图版。ＳＬＵＧ试井乘积图版分辨率高、灵敏度好、唯一性强,ＳＬＵＧ试井乘积曲线容易制作。ＳＬＵＧ试井乘积图版可用于一开、一开一关、二开二关、三开三关ＳＬＵＧ试井。  相似文献   

Approximate General Solution Of The Two-Dimensional Duffing Dynamical System     

K.?E.?PapadakisEmail author  G.?A.?Katsiaris  C.?L.?Goudas 《Astrophysics and Space Science》2005,300(4):297-328

This paper presents the approximate general solution of the triple well, double oscillator non-linear dynamical system. This system is non-integrable and the approximate general solution is calculated by application of the Last Geometric Theorem of Poincaré (Birkhoff, 1913, 1925). The original problem, known as the Duffing one, is a 1 degree of freedom system that, besides the conservative force component, includes dumping and external forcing terms (see details in the web site: http://www.uncwil.edu/people/hermanr/chaos/ted/chaos.html). The problem considered here is a 2 degree of freedom, autonomous and conservative one, without dumping, and of axisymmetric potential. The space of permissible motions is scanned for identification of all solutions re-entering after from one to nine oscillations and the precise families of periodic solutions are computed, including their stability parameter, covering all cases with periods T corresponding to 4osc/T. Seven sub-domains of the space of solutions were investigated in detail by zooming, an operation that proved the possibility to advance the accuracy of the approximate general solution to the level permitted by the integration routine. The approximation of the general solution, although impressive, provides clear evidence of the complexity of the problem and the need to proceed to larger period families. Nevertheless, it allows prediction of the areas where chaos and order regions in the Poincaré surfaces of section are to be expected. Examples of such surfaces of sections, as well as of types of closed solutions, are given. Two peculiar points of the space of solutions were identified as crossing, or source points from which infinite families of periodic solutions emanate. The morphology and stability of solutions of the problem are studied and discussed.  相似文献   

Identification of zones of preferential groundwater tracer transport using a mobile downhole fluorometer   总被引：1，自引：0，他引：1  

Raymond M. Flynn  Pierre-Andre Schnegg  Roberto Costa  German Mallen  François Zwahlen 《Hydrogeology Journal》2005,13(2):366-377

A mobile downhole fluorometer was used to detect zones of preferential groundwater tracer transport into an observation well. Identification of such zones is not possible if individual samples are collected over the wells entire screened interval. Laboratory-based tests using the fluorometer, and a purpose-built apparatus demonstrated that the fluorometer could be used with tracers to characterise well water flow regimes. During field investigations in a porous aquifer, the fluorometer monitored tracer concentrations in an observation well with a 12-m-long screen, 10 m down the hydraulic gradient from a fully penetrating injection well. Test results showed that the tracer occurred in the observation well over a discrete 2.5-m-thick interval. Single-well dilution test and vertical-flow data indicated that water entered the well at additional depths, but no tracer was detected at these levels. A numerical model reproducing dilution test concentration profiles indicated that water entered the well in many of these horizons at comparable velocities to those in the tracer-bearing zone. These data suggest that groundwater flow direction varied with depth in the aquifer under investigation. Moreover, simulations of tracer arrival indicated that the tracer distribution observed in the observation well was derived from a horizon that may be no thicker than 0.5 m.

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Resumen Se utilizó un fluorómetro móvil descendente para detectar zonas de transporte preferencial de trazadores de agua subterránea en un pozo de observación. La identificación de tales zonas no es posible si se colectan muestras individuales en todo el intervalo enmallado del pozo. En base a pruebas de laboratorio utilizando el fluorómetro y un aparato especial construido se demostró que el fluorómetro podría utilizarse con trazadores para caracterizar ambientes de flujo de agua en los pozos. Durante investigaciones de campo en un acuífero poroso, el fluorómetro monitoreó concentraciones de trazadores en un pozo de observación con una malla de 12 m de largo, 10 m abajo del gradiente hidráulico de un pozo de inyección que penetra totalmente el acuífero. Los resultados de las pruebas muestran que el trazador se presentó en el pozo de observación en un intervalo discreto de 2.5 m de espesor. Pruebas de dilución en un solo pozo y datos de flujo vertical indicaron que el agua entró al. pozo en profundidades adicionales, pero que no se detectó el trazador en esos niveles. Un modelo numérico que reproduce los perfiles de concentración de las pruebas de dilución indica que el agua entró al. pozo en muchos de estos horizontes en velocidades comparables a las existentes en la zona portadora de trazadores. Estos datos sugieren que la dirección de flujo de agua subterránea varió con la profundidad en el acuífero bajo investigación. Por otra parte, las simulaciones de llegada del trazador indicaron que la distribución del trazador observada en el pozo de observación se derivó de un horizonte cuyo espesor puede no ser mayor de 0.5 m.

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Résumé Un fluorimètre a été utilisé pour détecter les zones découlement préférentiel dun traceur dans un puits dobservation. Les identifications de telles zones nest pas possible si les échantillons individuels sont collectés sur toute les longueurs des parties crépinées du puits. Les tests de laboratoire utilisant un fluorimètre et un dispositif adéquat ont montré que les fluorimètres pouvaient servir à définir les régimes découlement de leau dans les puits. Durant les investigations de terrain dans un aquifère poreux, le fluorimètre a enregistré les concentrations du traceur dans un puits dobservation avec une crépine de 12 m. de long, 10 m sous le gradient hydraulique dans un puits à pénétration totale. Les résultats des tests ont montré que le traceur apparaissait dans un interval discret de 2.5 m de long. Un test de dilution en puits unique et des données découlement vertical ont indiqué que leau rentrait dans le puits à dautres profondeurs, mais le traceur na pas été détecté à ces niveaux. Un modèle numérique reproduisant le test de dilution et le profil de concentration a indiqué que leau entrait dans le puits à ces niveaux à des vitesses comparables de celle du traceur. Ces données suggèrent que lécoulement des eaux souterraines varie avec la profondeur dans laquifère sous la zone dinvestigation. Dailleurs, les simulations de larrivée du traceur ont montré que la distribution des concentrations du traceur dans le puits ne pouvaient pas être dues à une couche plus fine que 0.5 m.

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天然气水合物的测井识别和评价   总被引：14，自引：0，他引：14  

王祝文  李舟波  刘菁华 《海洋地质与第四纪地质》2003,23(2):97-102

地球物理测井作为传统的资源评价方法，在天然气水合物勘探中是有效评价手段。从国内外对天然气水合物的研究现状出发，简要地总结了天然气水合物的地球物理特征，介绍了利用电阻率测井和声波速度测井识别含天然气水合物储集层的方法和对天然气水合物进行评价，对现有的测井评价模型进行了讨论，指出了对天然气水合物储集层的地球物理测井评价模型还有待于进一步探讨。  相似文献   

对东明深井注水恢复试验的解释     

张昭栋  张继红  郑金涵  张广城 《地震》1995,(1):83-88

本文介绍了山东东明井的概况。1987年3月在该井进行了注水恢复试验,将该井含水层理想化为一无限水平承压含水层,根据H.H.Cooper等理论,对这次试验结果进行了处理,求出了东明井含水层的导水系数为8.7×10~9(m~2/s),这比一般含水层低得多。讨论了该井无“微动态”变化的原因,在于其含水层渗透性太差。 注水恢复试验方法为确定水井含水层的导水系数给出了一种简易可行的方法。有了这个系数,对井水位变化的分析提供了一种有用的参数。  相似文献