近海底磁异常得到的过去 780ka地磁强度变化     

Jeffrey  S.Gee  高丽萍 《海洋地质前沿》2001,17(3):19-21

古地磁强度波动可以正确地限定地球动力模式。对于５０ｋａ以来的偶极强度变化 ,已有充足的从古地磁和火山物质得到的绝对强度来加以说明 ,但是缺乏更早时期的这类资料 ,因而只能对其强度记录的最普通的特征做一测定。现在 ,沉积层序特别是布容正向期已提供出越来越多的相对古强度记录 ,然而就获取沉积物剩磁和什么标准化参数适合相对古强度的推断来说尚有许多不确定因素 ,再者根据绝对强度记录的最佳说明部分（全新世）对这些相对强度记录进行校准通常来说也是不可能的 ,这是因为最上部沉积物经常缺失或被扰动的缘故。海洋磁异常提供了用于…  相似文献   

三维层序地层学和与体系域有关的隐秘圈闭实例     

Reym.  BA 艾湘 《海洋地质译丛》1996,(3):57-64

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澳大利亚陆缘富硫化氢水合物和盐水流体     

高丽萍  侯贵卿 《海洋地质前沿》2001,17(6):16-18

澳大利亚南部陆缘为离散、被动陆缘 ,是在白垩纪导致澳大利亚与南极分离的拉伸和断裂时期形成的。现代陆架为无沉积物补偿陆架 ,这是因为虽然相邻的陆缘有很高的沉积速率 ,但是陆架区几乎没有沉积物堆积且晚第三纪晚期的岩石在地表出露。陆架的浅深度说明更新世时期陆架曾多次露出水面。大洋钻探计划（ＯＤＰ）１８２航次期间在２００～３９００ｍ水深处打了９个钻孔。所有钻位的样品长度为５～１０ｃｍ ,取样间隔约９．５ｃｍ。从这些样品中挤压出孔隙流体 ,利用ＯＤＰ标准程序进行盐度、Ｃｌ- 、Ｎａ+ 、Ｍｇ２ + 、Ｃａ２ + 、Ｓｒ２ + …  相似文献   

The dust distribution within the inner coma of comet P/Halley 1982i: encounter by Giotto's impact detectors     

McDonnell JA  Alexander WM  Burton WM  Bussoletti E  Evans GC  Evans ST  Firth JG  Grard RJ  Green SF  Grun E  Hanner MS  Hughes DW  Igenbergs E  Kissel J  Kuczera H  Lindblad BA  Langevin Y  Mandeville JC  Nappo S  Pankiewicz GS  Perry CH  Schwehm GH  Sekanina Z  Stevenson TJ  Zarnecki JC et AL 《Astronomy and Astrophysics》1987,187(1-2):719-741

Analysis of the data from Giotto's Dust Impact Detection System experiment (DIDSY) is presented. These data represent measurement of the size of dust grains incident on the Giotto dust shield along its trajectory through the coma of comet P/Halley on 1986 March 13/14. First detection occurred at some 287000 km distance from the nucleus on the inbound leg; the majority of the DIDSY subsystems remained operational after closest approach (604 km) yielding the last detection at about 202000 km from the nucleus. In order to improve the data coverage (and especially for the smallest grains, to approximately 10(-19) kg particle mass), data from the PIA instrument has been combined with DIDSY data. Flux profiles are presented for the various mass channels showing, to a first approximation, a 1/R2 flux dependence, where R is the distance of the detection point from the cometary nucleus, although significant differences are noted. Deviations from this dependence are observed, particularly close to the nucleus. From the flux profiles, mass and geometrical area distributions for the dust grains are derived for the trajectory through the coma. Groundbased CCD imaging of the dust continuum in the inner coma at the time of encounter is also used to derive the area of grains intercepted by Giotto. The results are consistent with the area functions derived by Giotto data and the low albedo of the grains deduced from infrared emission. For the close encounter period (-5 min to +5 min), the cumulative mass distribution function has been investigated, initially in 20 second periods; there is strong evidence from the data for a steepening of the index of the mass distribution for masses greater than 10(-13) kg during passage through dust jets which is not within the error limits of statistical uncertainty. The fluences for dust grains along the entire trajectory is calculated; it is found that extrapolation of the spectrum determined at intermediate masses (cumulative mass index alpha = 0.85) is not able to account for the spacecraft deceleration as observed by the Giotto Radio Science Experiment and by ESOC tracking operations. Data at large masses (>10(-8) kg) recently analysed from the DIDSY data set show clear evidence of a decrease in the mass distribution index at these masses within the coma, and it is shown that such a value of the mass index can provide sufficient mass for consistency with the observed deceleration. The total particulate mass output from the nucleus of comet P/Halley at the time of encounter would be dependent on the maximum mass emitted if this change in slope observed in the coma were also applicable to the emission from the nucleus; this matter is discussed in the text. The flux time profiles have been converted through a simple approach to modeling of the particle trajectories to yield an indication of nucleus surface activity. There is indication of an enhancement in flux at t approximately -29 s corresponding to crossing of the dawn terminator, but the flux detected prior to crossing of the dawn terminator is shown to be higher than predicted by simple modelling. Further enhancements corresponding to jet activity are detected around +190 s and +270 s.  相似文献   

<海洋地质与第四纪地质>引用外文期刊情况初步统计     

高丽萍 《海洋地质与第四纪地质》2000,20(4):98

我们采用文献计量学方法对1995～1999年<海洋地质与第四纪地质>所有文章引用的国外期刊文献作了统计(不包括增刊).该刊为我国海洋地质与第四纪地质的学术性刊物,我们选择该刊为调查依据,从中找出从事本学科专业研究的作者最常引用的外文期刊,即核心期刊,供广大读者参阅.  相似文献   

The phosphoric acid leak from the wreck of the MV Ece in the English Channel in 2006: Assessment with a ship of opportunity, an operational ecosystem model and historical data     

Kelly-Gerreyn BA  Hydes DJ  Hartman MC  Siddorn J  Hyder P  Holt MW 《Marine pollution bulletin》2007,54(7):850-862

This study evaluates the ship of opportunity (Ferrybox) concept for both sustained monitoring of UK shelf sea waters and numerical model validation. Release of phosphate from the wreck of a chemical tanker (MV Ece) in the western English Channel (49.73 degrees N, 3.25 degrees W) in March 2006 is used to demonstrate the importance of sustained observations in decision support systems and policy development. The Ferrybox system continuously collects sea surface (5m) data from a suite of autonomous electronic sensors installed on a passenger ferry operating year-round between Portsmouth (UK) and Bilbao (Spain). The detection of anomalously high concentrations of phosphate (1.54mmolm(-3), four times the usual level) and onset of phytoplankton growth close to the wreck site in March 2006 was placed in the context of multiple years of measurements (phosphate, nitrate, silicate and chlorophyll) collected from the Ferrybox system (2003-2006) and the long-term time series station E1 (50.03 degrees N, 4.65 degrees W, 1930-1987) in the English Channel. With regard to decision support, release of phosphate from the tanker is unlikely to pose a threat as phytoplankton growth at the end of winter is not unusual in this region and dissolved inorganic nitrogen rather than phosphate (DIN:DIP=10-18) is likely to ultimately limit algal growth in spring 2006. With regard to policy development, the Oslo and Paris (OSPAR) commissions recommendation of sampling every three years in "non-problem areas" is likely to provide statistically inadequate data, given the interannual and decadal variability identified in the Ferrybox and E1 data: the Ferrybox data show that oceanic winter nutrient concentrations varied by 35-50% between 2003/2004 and 2005/2006 due to deeper mixing of water off-shelf in early 2005/2006 and comparisons between the Ferrybox and E1 years show that the western English Channel is currently experiencing a low in phosphate concentrations similar to those in the 1960s. The importance of Ferrybox data in evaluating the reliability of predictive operational models needed in decision support is also demonstrated, by highlighting both strengths and weaknesses in a state-of-the-art ecosystem model designed for UK shelf waters.  相似文献   

北达科他州雷暴计划—高原雷暴的合作研究     

Boe  BA 高康 《山西气象》1994,(A04):70-82

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GM(0,2)模型在遥感估算区域降水中的应用          下载免费PDF全文

贺明慧  高丽萍  石宇虹  陶向新  孙华林 《气象与环境学报》2004,21(2):30-31

根据遥感植被指数信息 ,基于灰色累加生成原理 ,利用植被指数增长与旬累积降水量的同步性 ,建立旱年、正常年的GM (0,2)模型 ,归纳为 2种不同气候类型模式 ,并利用旬植被指数来估计旬降水累积量 ,可通过累减还原估算出旬降水量  相似文献   

Heterolocalism: an alternative model of the sociospatial behaviour of immigrant ethnic communities   总被引：2，自引：0，他引：2  

Zelinsky W  Lee BA 《International journal of population geography : IJPG》1998,4(4):281-298

"This paper evaluates critically the applicability of the well-known assimilation and pluralist models to the contemporary ethnic landscape of the U.S.... We then consider an alternative model, labelled heterolocalism, which suggests that members of certain newly arrived groups may be able to sustain their identity as an ethnic community despite immediate or rapid spatial dispersion. The applicability of the heterolocal perspective to non-metropolitan and transnational phenomena is evaluated in subsequent sections of the paper."  相似文献   

烃类矿床盖层中的次生矿化作用     

Б.  BA 王勋弟 《国外地质与勘测》1995,(4):14-17

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