认真学习贯彻十六大精神努力开创全省国土资源管理工作新局面

党的十六大高举马列主义、毛泽东思想、邓小平理论和“三个代表”重要思想的旗帜,提出了加快推进社会主义现代化建设,到2020年全面建设小康社会的奋斗目标,同时也对新时期国土资源工作指明了前进的方向,提出了更高的要求。国土资源工作是中国特色社会主义事业的重要组成部分,对我国实现全面建设小康社会的奋斗目标至     

贯彻十六大精神谱写国土资源工作新篇章

党的十六大确定的全面建设小康社会的宏伟目标,对各行各业的工作都提出了新的要求。作为国民经济建设基础性工作的国土资源工作,在全面建设小康社会的进程中起着致关重要的作用。而身为国土资源管理部门的领导,他们是如何把握和贯彻十六大精神的?围绕这一问题,《南方国土资源》杂志社特邀广西国土资源厅领导畅谈了未来对国土资源管理工作的思路和构想,现将其摘登如下,以飨读者。     

中央对国土资源管理工作提出新要求

江泽民同志在代表党中央所作的十六大报告中发出了全面建设小康社会，开创中国特色社会主义事业新局面的伟大号召，提出了全面建设小康社会的奋斗目标。胡锦涛同志在中央人口资源环境工作座谈会上强调，切实抓紧抓好人口资源环境工作，确保实现全面建设小康社会目标。同时中央对进一步做好新形势下的国土资源管理工作提出了新的更高的要求。本刊摘登中央领导有关国土资源的论述，以便国土资源战线的工作人员深入学习贯彻党的十六大和中央人口资源环境工作座谈会精神。     

用十六大精神指导国土资源工作

刚刚闭幕的党的十六大,是我们党在新世纪召开的第一次代表大会,也是我们党在开始实施社会主义现代化建设第三步战略部署的新形势下召开的一次十分重要的代表大会.当前,摆在我们面前的首要任务,就是要认真学习十六大报告,认真贯彻十六大精神,扎实工作,奋发进取,把思想和认识统一到十六大报告精神上来,把智慧和力量凝聚到实现十六大提出的任务上来.     

持续提高国土资源法制化水平

正党的十八届四中全会就全面推进依法治国若干重大问题作出一系列重大部署,为坚持走中国特色社会主义法治道路、建设中国特色社会主义法治体系、建设社会主义法治国家指明了方向。各级国土资源主管部门要吃透精神、狠抓落实,运用法治思维谋划推动国土资源改革,通过改革加快完善国土资源法治体系,进一步提高国土资源管理法治化水平。全面推进依法治国,是完善和发展中国特色社会主义制度、推进国家治理体系和治理能力现代化的重要工作。     

与时俱进开拓创新努力开创全省国土资源工作新局面--在全省国土资源工作会议上的讲话

同志们: 这次全省国土资源工作会议,是在全省上下认真贯彻党的十六大和全国“两会”及省十次党代会精神,为实现“建设小康,富民强省”目标而努力奋斗的新形势下召开的一次重要会议。今年3月9日,在中央人口资源环境工作座谈会上,胡锦涛总书记发表了重要讲话,对国土资源工作提出了新的要求,对今后的工作具有重要的指导意义。过去几年,在省委、省政府和国土资源部的正确领导下,全省国土资源系统广大干部职工奋     

2003年江苏省国土资源工作要点

2003年,全省国土资源工作的指导思想是:以邓小平理论和"三个代表"重要思想为指导,认真学习贯彻党的十六大、中央和全省经济工作会议精神,坚持保护资源的基本国策,以服从大局、服务中心、保护资源、保障发展为总要求,以增强对经济社会可持续发展的保障能力为目标,以维护广大人民群众利益为根本出发点,以改革创新为动力,以信息化和基础业务建设为支撑,以加强队伍建设为重要保证,全面推进依法行政,努力提高国土资源调查、规划、管理、保护和合理利用水平,为全面建设小康社会和在我省率先基本实现现代化作出新的贡献.     

认真学习贯彻十六大精神努力开创河南国土资源事业新局面

全党全国人民极为关注的党的十六大已经胜利闭幕。这次大会是我们党在新世纪召开的第一次代表大会，也是我们党在开始实施社会主义现代化建设第三步战略部署的新形势下召开的一次十分重要的代表大会。江泽民同志在大会上所作的报告，全面分析了我们党面临的国际国内形势，科学总结了十三年来的基本经验，进一步阐述了“三个代表”重要思想的历史地位和贯彻“三个代表”重要思想的根本要求，深刻阐明了我们党在新世纪举什么旗、走什么路、实现什么目标等重大问题，对建设中国特色社会主义经济、政治、文化和党的建设等各项工作做出了全面部署…     

解放思想与时俱进努力开创国土资源管理工作新局面

党的十六大指出:“坚持党的思想路线,解放思想,实事求是,与时俱进,是我们党坚持先进性和增强创造力的决定性因素。与时俱进就是党的全部理论和工作要体现时代性,把握规律性,富于创造性。”当前,我国已进入全面建设小康社会新的发展阶段。在这形势迫人的情况下,我们国土资源部门应结合自己的实际,努力塑造国土资源管     

十六大报告中有关国土资源的论述

党中央对国土资源工作非常重视和关切,在党的十六大报告中,多处论述了国土资源工作。这些论述是新时期国土资源工作创新与发展的行动指南和奋斗目标。为了促进十六大精神的深入学习贯彻,现将有关论述摘刊出来,以使广大国土资源工作者及相关读者学习之用。     

四川盆地珍珠冲组植物群特点及侏罗系与三叠系界线的厘定

归纳总结了四川盆地珍珠冲组植物化石7类50属128种,须家河组植物化石10类71属267种,并将珍珠冲组植物群划分为上、下两个组合.通过分析两组植物群的发育特点及演化规律,结合区域有关资料,对侏罗系与三叠系界线进行了厘定.在四川盆地北部大巴山前缘地区,依据珍珠冲组(白田坝组)的岩性特征和所含植物化石特征,将侏罗系与三叠系的界线置于含Coniopteris植物化石的珍珠冲组(白田坝组)底部石英质砾岩或石英砂岩之下的假整合面或剥蚀面上;在四川盆地东北部的云阳、奉节及长江以南万县地区,侏罗系与三叠系的界线划在云阳南溪剖面上含Coniopteris murrayana植物化石8.3 m之下的珍珠冲组黄绿色泥质粉砂岩夹粉砂质泥岩地层之底.     

古代雷州半岛海神信仰略析

古代,雷州半岛信仰的海神主要有伏波将军和妈祖,尤其是元代以后,妈祖影响超过伏波,这主要有三方面原因:1)妈祖得到上层统治阶级的青睐,2)雷州半岛的汉人多为福建移民,3)雷州半岛少数民族的外迁。     

Contrast between the climatic states of the warm pool in the Indian Ocean and in the Pacific Ocean

Based on the analysis of Levitus data, the climatic states of the warm pool in the Indian Ocean (WPIO) and in the Pacific Ocean (WPPO) are studied. it is found that WPIO has a relatively smaller area, a shallower bottom and a slightly lower seawater temperature than those of WPPO. The horizontal area at different depths, volumes, central positions, and bottom depths of both WPIO and WPPO show quite apparent signals of seasonal variation. The maximum amplitude of WPIO surface area’s seasonal variation is 58% larger over the annual mean value. WPIO’s maximum volume variation amplitude is 66% larger over the annual mean value. The maximum variation amplitudes of the surface area and volume of WPPO are 20.9% and 20.6% larger over the annual mean value respectively. WPIO and WPPO show different temporal and spatial characteristics mainly due to the different wind fields and restriction of ocean basin geometry. For instance, seasonal northern displacement of WPIO is, to some extent, constrained by the basin of the Indian Ocean, while WPPO moves relatively freely in the longitudinal direction. The influence of WPIO and WPPO over the atmospheric motion must be quite different.     

Changes in the thermal and hydraulic regime within the active layer in the Qinghai-Tibet Plateau

The change trends of air temperature,precipitation and evaporation from 1999 to 2008 shows that the climate in the Qinghai-Tibet Plateau permafrost region had become warmer.The analysis of the systematic active-layer data monitoring network along the Qinghai-Tibet Highway indicated that the active-layer thickness had been increasing and the soil temperature was rising.The soil temperature was rising in winter but not at the end of spring or during the entire summer.With thickening and warming of the active layer,the liquid water content of the active layer had an obvious downward migration and liquid water content in the top horizons decreased,but in the deeper horizons it increased.     

The influence of the sea-air heat exchange over the Kuroshio in the East China Sea in winter on the precipitation in the middle and lower reaches of Changjiang River in flood season

In this paper, the sea-air heat exchange over the Kuroshio in the East China Sea during the winters of 1954–1972 is computed and analysed. The results indicate that the year to year anomalies of sea-air heat exchange are obvious and the values are mainly controlled by the intensity of the cold air at the same time. The authors have found a close relationship between sea-air heat exchange and precipitation in the region of the Changjiang River during the early summer. Finally, the predicting indication for forecasting this precipitation around the middle and lower reaches of Changjiang River in June is given. Contribution No. 839 from the Institute of Oceanology, Academia Sinica. This paper was published in Chinese inOceanologia et Limnologia Sinica 14 (3): 256–262, 1983.     

Characteristics of the transition Layer in the South China Sea in 1998

CTD data on standard levels coolected during July and December in 1998 and the cubic spline interpolating method were used to study the characteristics of the transition layer temperature and salinity.The thermocline undergoes remarkable seasonal variation in the South China Sea (SCS),and especially in the region of the north shelf where the thermocline disappears in december.The thermocline is stronger and thicker in July than in December,There is no obvious seasonal variation in the halocline.Due to the upper Ekman transport caused by monsoon over the SCS,the thermocline slopes upward in July and downward in december from east to west in the northern SCS.The characteristics of the thermocline and halocline are influenced by local eddies in the SCS.The Zhujiang diluted flow influences significantly the SCS shelf‘s halocline.     

鱼虾混养池中蓝藻群落结构及其微囊藻毒素含量变化

对广东省中山市三角镇的低盐度鱼虾混养池进行连续采样分析,结果表明,混养池中的蓝藻主要有螺旋藻(Spirulina sp.),鱼腥藻(Anabaena sp.),颤藻(Oscillatoria sp.)、铜绿微囊藻(Microcystis aeruginosa)等,其中盐泽螺旋藻的优势度为0.52~0.73。蓝藻是水体中的优势微藻种群,蓝藻细胞数量占微藻细胞数量的88%~99%,蓝藻细胞数为0.99×10~9~5.89×l0~9 cell/L。混养池微藻多样性指数(H’)为1.16~2.49,养殖水体处于中度污染状态。溶解性无机氮的质量浓度为0.13~2.30 mg/L,正磷酸盐质量浓度为0.25~2.39 mg/L,化学需氧量的质量浓度为1.94~13.79 mg/L。微囊藻毒素(MC-LR)在水中质量浓度为0.18~0.79μg/L。蓝藻细胞数量与化学需氧量之间呈显著的正相关关系,表明蓝藻的生长情况与养殖池中的有机污染程度有密切联系,低盐度的富营养化的水体能促进蓝藻的生长,成为微藻群落中的优势种群。MC-LR的质量浓度与蓝藻细胞数量之间无显著相关。     

Changes in the network of tourist trails in the border zones of the Czech Republic after entering the Schengen area

Among the factors influencing tourist trail network development are political issues, including the presence of state borders, the possibility of crossing them and the accessibility of border zones. In the article, it was decided to look at changes in the offer of tourist trails(hiking and cycling) along the entire border of the Czech Republic after the extension of the Schengen area(within this area, crossing the border is possible anywhere, and not only at official border crossings). It should be emphasized here that the borders of the Czech Republic over most of their length run through mountainous areas and, apart from political factors, natural features should have a major impact on the development of tourist routes. In order to determine the coherence of the current network of trails on both sides of the Czech Republic state border, modern tourist maps have been analyzed, determining the number of places where it is possible to cross the state border with the help of a marked tourist trail. Based on that, two indicators were introduced to determine the degree of openness with all neighboring countries as regards the opportunity to cross on a tourist trail. Changes in the historical situation, a comparison of the accessibility of the border area before entering the Schengen area and 2019, were analyzed for two study areas using archival maps. Over a decade after the extension of the Schengen area, the number of places where tourist trails of neighboring countries approach the border has clearly increased. Crossing is more often made possible using hiking trails than cycling routes(trails of the first type cross the border every 7.91 km, while the latter every 13.3 km), but considering the speed of movement, it can be assessed that the openness for cyclists is higher than for hikers. Moreover, in many places there is still significant potential for further integration of tourist trail networks as trails created in one country often do not have a continuation on the other side of the border.     

Modeling the ocean circulation in the Bering Sea

With parameterized wave mixing, the circulation and the tidal current in the Bering Sea were simulated simultaneously using the three-dimensional Princeton Ocean Model. The simulated circulation pattern in the deep basin is relatively stable, cyclonic, and has little seasonal change. The Bering Slope Current between 200-1000 m isobaths was estimated to be 5 Sv in volume transport. The Kamchatka Current was estimated to be 20 Sv off the Kamchatka Peninsula. The Bering shelf circulations vary with season, driven mainly by wind. These features are consistent with historical esti- mates. A counter current was captured flowing southeastward approximately along the 200 m isobath of the Bering Slope, opposite to the northwestward Bering Slope Current, which needs to be validated by observations. An upwelling current is located in the shelf break （ 120-1000 m） area, which may imply the vertical advection of nutrients for supporting the Bering Sea Green Belt seasonal plankton blooms in the breakslope area. The Bering Slope Current is located in a downwelling area.