下面是小编为大家整理的2023年自然资源人才强国交流材料五篇,供大家参考。希望对大家写作有帮助!
自然资源人才强国交流材料5篇
第一篇: 自然资源人才强国交流材料
人才强税战略经验交流材料与人才行动工作计划汇编
人才强税战略经验交流材料
一、新形势下对纳税服务工作的再认识和定位
一是要充分认识纳税服务工作的重要性。纳税服务是税收征收管理工作的有机组成部分，是贯穿税收征管全过程的基础性工作。纳税服务伴随税收管理，服从和服务于税收征管工作，也是提升全社会纳税意识。纳税服务从税前、税中、税后参与税收管理服务。税前为纳税人提供咨询和服务，以提高纳税人履行纳税义务的意识；
税中为纳税人服务，使纳税人能够更方便、快捷、准确地履行纳税义务；
税后为纳税人服务和提供方便。
二是要准确定位纳税服务的工作职责。纳税服务是依法行政不可缺少的一部分，更是服务型政府为公众提供服务的法定应尽义务和职责，是税务机关的责任和义务。国家税务总局将纳税服务工作的主要职责归纳为“十六个字”“税法宣传、纳税咨询、办税服务、权益保护”。作为为纳税人提供的公共服务，税务工作者纳税服务遵循无偿、平等、公平、效率的原则。
三要按照正确的纳税服务的理念。根据纳税人的需求、让纳税人满意是纳税服务的工作理念。目标是促进纳税依法纳税，提高税收征管质量和效率、保护纳税人合法权益，努力实现税收管理的社会效益最大化。
二、税务人才是强税的重要资源
在现实社会中，科技发展和创新已成为经济增长的不竭动力，随着税收征管信息化进程的加快，对税收业务专业人才的要求也就越来越高，税务专业人才在税收发展中的地位和作用也日益突出。一是税务人才是科技兴税最主要的推动力和开拓者。任何一项科学技术的进步都是由掌握了丰富实践知识并具有创新精神的人才实现的。税务人才也一样，从手工开票到征管软件的开发利用，从上门收税到网上报税，无一不是税务人才推动着税收征管一步一步走向现代化、信息化。二是税务人才是社会主义税收事业持续发展的组织者和指挥者。从现实生活中我们认识到，税收任务年年超额完成，税收职能的日益完善都需要税收管理者正确的决策和正确的指挥。俗话说“鼓敲千遍，一锤定音”，也说明了税务管理人才对税收事业的发展起着举足轻重的作用。三是税务人才是税收资源的开发者和利用者，是税收资源中最宝贵的资源。税务人才具有其他税收资源所没有的自主性、能动性和创造性，居于主导、决定地位。税务人才资源的开发和利用是一切税收资源开发利用的前提和基础。没有对社会保障体系的研究，就不可能开征社会保障税，没有对固定资产投资拉动地方经济发展的研究就不可能停征固定资产投资方向调节税。所以，只有税务人才发挥能动作用时，税收资源才能跟着发挥作用。
税收和经济的发展是相辅相成的，互相作用。地方经济的发展必须依靠税收支撑，税收事业的发展则需要精通税收业务的专业性人才支撑。近年来，我们不断深化人事制度改革，把好入口关、抓好培训关，取得了显著成绩，也初步形成了税政、电脑、稽查、写作等专业人才队伍。但总的来看，我们还面临着严峻的考验。如何抓住机遇，迎接挑战，下大力气抓好税务人才的培养开发，创造出人才辈出、人尽其才的可喜局面，已成为摆在我们面前的一项重大而紧迫的战略任务，所以说人才是抢谁的关键。
三、推进税务专业人才整体开发
俗话说，十年树木，百年树人，讲的就是人才相当重要的道理。税务系统专业性很强，面貌能不能改变，事业能不能发展，关键在于有没有一批可用的人才，尤其是地税系统，人少税种多,征管范围大,要增强地税发展的核心竞争力，关键在于人才资源的整体开发。
实施人才强税战略，推进税务人才整体开发，必须抓住人才培养、吸引、使用三个环节，着力建设好管理型、专业型人才两支队伍，重点抓好高层次人才培养。要坚持以税务人才资源能力建设为主题，以挖掘现有人才潜力为基础，以促进地方经济和税收事业发展的需要为出发点，通过多种方法和途径，重点培养人才的创新精神，开发人才的创新能力。目前，我国迎来了又一轮经济发展高潮，为各种投资发展提供了广阔的天地，税收政策、制度对企业经营影响也日益突出，这就更需要我们拥有专业型、复合型高素质的税务人才不断创新征管手段，不断提高税务信息化水平，以应对各种新情况、新问题。因此，我们要有重点地培养专业型人才，选择复合型人才，实行重点带动，整体推进，推动税务人才队伍建设的全面发展。同时，还要创新税务人才使用机制，坚决冲破一切妨碍人才发展的思想观念，要充分利用现有人才资源，建立健全人才竞争激励机制，确保人尽其才，能上能下，增强用人制度的活力，充分调动各类专业人才的积极性和创造性。要建立健全人才资源优化配置机制，充分发挥人才在税收工作中的基础性作用。要大胆选拔启用税务高素质人才，努力营造“尊重劳动、尊重知识、尊重人才、尊重创造”的良好环境，促进形成关心、爱护、理解、信赖人才的社会氛围，充分发挥人才的积极性和创造性，激励各类人才发挥聪明才智，为增加地方税收。
在实际工作中，领导全力主抓税务人才。领导重视、认识深刻，国税局人才培训工作能够长期坚持的关键因素。税务机构系统没有自己专门的培训场所、培训机构和固定的师资队伍，这严重制约了人才培训工作的正常开展。对此，国税局下大力气改变人才现状。根据国税系统人才培训的实际情况进行深入调研，明确了搞好税务人才培训工作的新理念，即增强“一个观念”,坚持“两个原则”,实现“三个转变”,走出“四个误区”，抓好“五项工作”。国税局把人才培训作为一项重要工作列入年度工作计划，做到与税收工作一起研究、一起部署、一起检查,突出了人才培训工作的基础性和重要性。不但如此,培训机构等基础设施建设也逐步完善。
国税局主管培训工作，要根据国税系统人才培训的实际情况进行深入调研，明确了搞好税务人才培训工作的新理念,即增强“一个观念”,坚持“两个原则”,实现“三个转变”,走出“四个误区”,抓好“五项工作”。步形成了“一把手”挂帅，领导班子配合分管主抓，业务处室承办，系统上下联动齐抓共管的人才培训工作格局。国税局把人才培训作为一项重要工作列入年度工作计划，做到与税收工作一起研究、一起部署、一起检查，突出了人才培训工作的基础性和重要性。
注重实效,提高实战能力。充分调动国税系统人才工作者参与人才培训工作调研的积极性，确定调研课题，安排部署国税系统人才部门结合实际，对人才培训工作中的热点、难点以及如何改进和提高人才工作实效等问题进行深入调研，形成调研成果，以指导全国税系统人才培训工作的有效开展。
建设“人才仓库”。在实施人才兴税战略的过程中,国税局通过层层选拔，严格考核，建立起国税系统的“人才仓库”。“人才仓库”在税务稽查、反避税、纳税评估等方面发挥了积极而重要的作用。因势利导，盘活人力资源。在基层,干部的年龄结构、知识结构亟待优化,新技术应用困难等现象比较普遍，通过培训,优化知识结构，提高计算机应用水平”的理念。这一理念引起了基层从事税务工作时间较长的干部职工的共鸣。当地国税局因势利导,大力开展应用培训。许多基层干部职工十分珍惜培训的机会，变要我学为我要学，在工作实践中积极学习新知识。
国税人才的政治素质和理论水平有了较大提高，业务素质和业务能力不断提高，文化结构和专业结构得到明显改善，执法水平、服务水平、管理水平明显提升，岗位能力持续提高。国税人才取得了多项卓越的工作业绩。国税局充分整合信息资源,今年初开发了税收管理员小助手软件,在推广后得到税务人和企业的普遍认可，多数人认为这是“两个减负”的好帮手。国税局推行通办办税模式。
四、加强对国税税法的大力宣传
在新形势时下，提高企业对国税税法的知晓率，积极开展国税税法的宣传活动，采取多形式、多途径地开展国税税法的宣传，推动和促进全社会国税税法业务的开展。一是定期开展全社会国税税法的宣传培训，请有宣传税务和法律部门的专家讲课；
二是利用电视、网络、报刊宣传国税税法的发展和服务工作；
三是建一批生活实用的宣传税法标志，编写一些短信宣传国税税法业务的语句；
四是把税务部门的业务宣传到窗口平台，做到来有应声，去有送声；
五是举办国税税法系统的文艺晚会，全社会宣传税法的服务社会各界的政策，广泛宣传国税税法的业务工作；
六是在服务窗口印发一些宣传单，做到家喻户晓，人人皆知；
七是每年向社会举办一次我与国税税法征文，对税法进行宣传；
八是每年在全社会开展一次国税税法有奖问答活动。让全社会各界知晓国税税法，在中国遍及城乡的税法业务发展体系，迅猛宣传国税税法。从而促进了税收，发展了国民经济，便收税为自觉纳税。
五、做好国税秘书日常工作、办文办事
随着信息论的兴起，现代社会进入了一个全新的“信息时代”。互联网是个庞大的互连系统，网上的资源非常丰富，涉及到人们的各个领域、行业及社会公共服务等方面。在新闻媒介、学术交流、税务数据库检索、迅速及时地传播各种信息。
作为领先于时代的税务秘书必须从工作方法上改变领导的观念，率先使用先进的工作平台，并确实带来实际效果。税务秘书工作的内容应不断拓展，秘书工作制度不断完善，作为税务部门秘书运行机制不断优化。不管是经验丰富的老税务秘书还是刚入行的新秘书都需要不断更新知识。税务秘书要求学会使用计算机技能。
一是税务秘书在网络技术高度发达的现今，首先要懂得透过网络收集信息，做好文件的传达。税务秘书在网络的大环境下出了要懂得利用网络收集信息外，还要懂得如何利用网络发送、传递信息。
办公自动化系统有助于提高税务秘书的工作效率，简化办公过程，及时、快捷的接受或发送信息。就是使用电子邮件和即使通讯工具收发信息、信函或是各类办公文件。
二是网络环境下个各种新兴产业也要求税务秘书在工作中能了解并运用到实际工作中。
网络的发展，互联网技术的应用，税务秘书作为一种广泛的社会职业，所承担的工作也越来越广泛，面临着前所未有的机遇和挑战。因此，要成为一名精明、能干的税务秘书一定要顺应历史潮流，跟上时代的快节奏步伐，扩展知识面，在工作中为人为文两从容，当好领导的参谋和助手。取用最少的时间，最便捷的方式带来最大的效益，出色的完成工作。
因此说税务的发展关键是人才。在实施专业化管理模式下，大力推进人才强税战略是非常重要的。
人才行动工作计划
在区委、区政府的正确领导下，在全区各部门的协同努力下，《-年区人才工作行动计划》已顺利实施完成，根据《市“”人才发展规划纲要》以及《区“”人才发展规划》精神，提出我区年人才工作行动计划。
一、指导思想
年人才工作将高举中国特色社会主义伟大旗帜，深入贯彻落实党的精神，坚持以邓小平理论和“三个代表”重要思想为指导，牢固树立科学发展观和科学人才观，按照中央和市委工作部署，大力实施科教兴区、人才强区战略，围绕区域经济社会发展，坚持党管人才原则，按照人才工作“2+1”的工作布局，全面加强人才工作机制建设，重点抓好人才工作队伍建设，切实做好人才工作基础建设，为实现经济实力更强、城乡环境更美、人民生活更好、社会更加和谐的目标提供智力支撑和人才保障。
二、工作目标
围绕我区“”人才发展规划提出的“到年，基本建成与区域功能及产业布局相协调、具有一定的区域辐射力和特色的实用人才集聚地，使成为精品钢铁、现代物流、高新技术、循环经济、现代农业等各类产业优秀专业人才的集聚之地、创业之地，培养造就一支与全区经济社会发展和城区功能定位相适应、数量充足、结构合理、素质优良、门类齐全的人才队伍”的总体目标，进一步完善人才成长的综合环境，进一步实施重点人才开发培养，进一步营造人才工作良好氛围。
三、主要任务
今后三年，在现有的产业发展和人才工作的基础上，围绕的经济社会发展，进一步加强人才工作的组织领导，扎实有效地做好我区“2+1”人才工作，推进实用人才集聚地建设。
（一）人才工作机制建设——进一步完善人才成长的综合环境，加强党对人才的领导
按照党管人才原则，形成管宏观，管政策，管协调，管服务的组织保障机制和工作责任机制，不断深化区委统一领导，“一把手”抓“第一资源”，组织人事部门牵头抓总，有关部门各司其职，社会力量广泛参与的人才工作格局，使党管人才的领导体制和组织体系建设不断得到延伸和发展。
进一步落实党管人才的工作机制。进一步深化和完善人才工作的各项制度。充分发挥人才工作协调小组作用，认真落实人才工作协调小组职责、目标和任务。进一步发挥人才工作协调小组办公室职能，重点做好对人才工作谋篇布局、指导管理。进一步完善区人才工作联络员制度，建立通畅的信息沟通和反馈机制。各级党委要落实好责任，统筹协调，形成“一把手”抓“第一资源”的工作格局。加强人才工作干部队伍建设，加大对人才工作干部队伍的专业培训力度。
进一步健全人才工作的管理服务机制。加强对人才工作的目标管理考核，对各单位的人才规划落实情况，人才培养、引进、使用情况进行考核，形成对人才工作长效、稳定的监督考核制度。加大人才工作资金投入力度，各单位要落实相应的人才工作资金，充分发挥资金扶持、奖励、资助、解困等作用。创新人才激励制度，逐步加大对高层次人才的政府补贴，奖励在本区经济、科技、社会领域做出突出贡献的先进单位和优秀人才，进一步激发人才的工作积极性和主动性。
进一步推进人才服务业发展机制。努力探索人才市场和劳动力市场的对接，从信息共享入手，加强人才市场与劳动力市场的贯通，构建统一、开放的人才资源市场体系。提高公共人事服务质量，重点推进人事代理、人才引进、人才测评以及发布人才供求信息等服务工作。创新人才柔性流动方式，制定和完善人才引进的各项政策，积极探索以兼职、咨询和技术合作等方式进行的人才引进方法。
（二）人才工作队伍建设——进一步实施重点人才开发培养，加强人才工作项目化管理
按照科学人才观的要求，以能力建设为核心，实施重点人才开发与管理，加快优秀人才向我区重点领域集聚，并以人才工作项目化的方式，指导和推进各单位人才队伍建设。
抓好党政领导人才队伍。规范领导干部选拔任用工作，大力推进党政机关领导干部公开选拔、竞争上岗和选调交流。进一步落实党政领导干部试用期制度、职务任期制度、辞职制度、选拔任用责任追究制度、任职回避制度。进一步加强党政领导干部的培养、储备，继续做好后备干部挂职锻炼工作。坚持做好新招录公务员基层锻炼工作，开展“岗位练兵”活动，提高公务员专业素养。
造就高层次专业技术人才队伍。加强适应区域经济社会发展需要的高层次和紧缺人才队伍建设，努力通过三年的时间，在各领域形成一支专业匹配、结构合理，具一定规模的人才梯队。重点抓好教育、卫生、文化系统的高层次专业技术人才，教育系统重点实施人才素质提升工程[i]；
卫生系统重点实施“2616”人才培养工程[ii]；
文化系统要建设一支结构合理、数量充足，专业特色强、整体素质较高，具有浓郁特色的文广人才队伍。努力建立高素质、社会化的专业技术人才队伍，提高专业技术人才的科学素质和创新能力，重点培养、引进和使用一批钢铁、物流、港口等生产性服务业及推进国际节能环保服务园、科技园、国际研发总部基地等重点项目急需的专门人才。以专业一流、团队优秀、项目领先为标准，在专业技术人才和企业经营管理人才中，培育一批领军人才，重点打造一支社会事业、现代生产服务业和高新技术企业的领军人才队伍，推进以领军人才为核心的创新团队申报承担国家、市、区的重大项目和重大研究课题，充分发挥领军人才的辐射作用和带动效能。
振兴高技能人才队伍。加快培养一支符合专业特色、数量充足、结构合理的高技能人才队伍。加强对职业培训市场的研究和技（职）校师资力量建设，改进技（职）校教学课程，建立技工见习（实习）基地。扩大委托培养规模，提高企业职工教育培训质量。通过开展技能竞赛活动，表彰有突出贡献的高技能人才，促进职工岗位成才。
探索成立社会工作人才队伍。进一步加强社会工作人才队伍建设基础研究，制定培养规划。实施“大学生进社区”计划，招录大学生充实到社区工作。开展区社会工作者专业培训，提升社会工作人才能力素质，促进社会工作专业化、职业化建设。依托“为民地图”工作，加强基层党群工作人才队伍建设及志愿者的培养和实训，提升服务质量。
加快打造农村实用人才队伍。继续做好“三支一扶”工作，深化“村村有大学生”计划的工作措施。研究出台进一步加强农村实用人才队伍建设的意见，开展农村实用技术培训，提高农民的科技素质和技能；
进一步加大政策扶持和人才扶持力度，使农村有一批留得住、用得上的人才。加强农村科技、教育、文化、卫生、经营管理等多方面的实用人才开发，重点培养一大批生产能手、能工巧匠、经营能人。
建设高素质经营管理人才队伍。进一步拓宽经营管理者眼界，培养全球性视野，探索、改进经营管理人才培训班的方法与内容，举办高级经理理论培训班和赴港实务培训班。推荐更多的经营管理人才参加中央党校、市委组织部及其他各类培训班和参观考察活动。对非公有制企业加大人才培养、成长政策上的关心和扶持，通过政策支持引进人才，鼓励人才带项目，项目带人才。加大对企业自主创新的科技资金与人才资金的支持。表彰纳税先进和有突出贡献的经营管理人才。建立中小型企业科协组织，进一步增加中小型企业科技人员的凝聚力。
（三）人才工作基础建设——进一步营造人才工作良好氛围，加强对人才工作的保障
夯实人才工作的基础，完善人才工作平台建设，实现人才资源信息共享，为人才施展才华提供宽广的发展舞台和必要载体。广泛宣传优秀人才先进事迹，发挥人才引领作用，通过营造良好的工作、生活、创业等环境，为人才的发展提供保障。
不断完善人才工作平台建设。做好第六批拔尖人才、青年尖子评选活动和培养、管理等工作。不断改进和完善人才服务的措施，开展健康体检、学术度假和出国培训考察等。通过每年开展优秀专家成果展示、出版专著等形式多样的活动，进一步发挥人才的聪明才智。积极创造条件，鼓励专业人才知识更新。加强高级专家协会和青年人才协会，充分发挥协会的自治作用，提升协会凝聚力。围绕经济社会发展的热点、难点问题，开展“讲坛”、论坛讨论、献计献策等活动。推进“三区联动”工作，继续开展暑期优秀大学生赴挂职实践活动及大学生见习基地建设工作。深化博士后创新实践基地建设，采用多种形式加强政策宣传，激励更多企业积极申报博士后科研项目，通过举办博士后成果展示会、博士后座谈会等方式，积极总结博士后创新实践基地工作经验，进一步扩大博士后创新实践基地的人才示范效应。继续加强留学人员创业园建设，构建多元化的留学回国人员创业资助和融资平台，构建符合海外人才发展特点的服务平台，吸引高层次留学回国人员创业发展。
扎实推进人才工作规范化建设。健全全区统一的人才资源库，囊括全区所有单位、部门的人才信息，实现全区人才流动、服务和管理的信息化。建立覆盖全区的人才统计机制，定期对人才需求进行科学预测，及时发布人才需求信息。完善人才考核档案，建立专业技术人才考核档案，将每年的考核情况完整记录，作为人才提拔、晋升、奖励的主要依据。做好人才队伍现状、紧缺人才的培养以及人才培养成长规划的调查研究，制订符合我区产业发展方向、体现经济发展特点的《人才开发目录》，切实做到底数清、情况明，紧贴实际，努力打造顺应发展需要的人才队伍。
努力扩大人才工作的宣传效应。大力宣传优秀人才的先进事迹和人才工作的先进经验，扩大关心、支持、参与实用人才集聚地建设的社会认同，确立人人争做贡献、人人立志成才、人人都能成才的社会舆论导向。强化人才强区战略的宣传效应，将人才宣传计划纳入全区宣传工作计划中，确定阶段性人才工作的宣传主题。积极宣传科学的人才观、“人才资源是第一资源”、“一把手”抓“第一资源”的观念。建立和完善人事人才网站，利用网络优势加强对高级人才的管理和服务；
以网络博客、人才为民服务等形式宣传人才，让社会认识人才、了解人才。继续做好《人才工作》期刊工作，力求在制作上的精益求精和发行上的广泛深入。
事以才成、业以才兴、区以才立。发展与进步的历程印证着人才是决定事业兴衰成败的关键之一，人才问题是关系党和国家事业发展的关键问题。做好人才工作，搞好人才队伍建设，更是组织工作的重要组成部分。我们要牢固树立科学发展观和科学人才观，坚持党管人才原则，调动和发挥各方的积极性和创造性，凝聚各阶层的智慧和力量，将区的人才工作推向新的高度。
第二篇: 自然资源人才强国交流材料
支部书记交流发言材料人才工作交流发言材料
通过企业靠前、搭建平台、优化服务等举措,***人才工程成效显著.截止目前,我县***人才工程000个岗位中,已完成00个岗位,共引进各类人才000人,其中领军人才1人,高级管理人才000人,高端专业人才000人.
我们的主要做法是：
一、突出企业为主,最大程度扭住牛鼻子企业入库.企业是人才集聚的主阵地,才智发挥的主战场.
建立***县科技企业库,综合考评人才规模、科研经费投入、研发平台搭建、引才活动参与等因素,将具有高层才人才20人以上的企业优先入库.入库企业引进1名高层次人才获得5000元奖励,优先享受政府投融资担保,科研经费投入纳入企业成本,同时优先申报科技和人才项目.
目前00家***人才工程企业中,有00家为入库企业,引进领军人才1人,高端专业人才3人,00家企业获评***明星企业.组团引才.
根据***人才工程人才需求,分条线组织00化工、00化工等00家化工企业组团赴哈尔滨工业大学、大连理工大学、南京工业大学专场招聘.组织00科技、00食用菌等农口企业赴南京农业大学、000招聘会.
组织县医院、00医院赴山东大学、扬州大学等高校现场招引卫技人才.目前,引进高层次人才68人.
其中,8人参加博士集聚计划面试答辩、3人参加双创面试答辩、新增省333工程3人.人才升值.
为人才提供成长成才空间,是企业最大的引力所在.鼓励、支持企业营造企业文化,创造人才个性化的升值空间,提供优良的工作环境.
目前,已有00、00等00家企业拥有自己的企业文化,建立企业文化宣传室.引进的高层次人才直接进入人才数据库,发放人才积分卡,享受创办企业、社会保险、医疗保健、职称评定、配偶就业、子女入学、住房保障等10项全方位、一站式服务.
二、突出服务为先,最大程度搭建快车道调研需求.及时转换政府角色,做好服务.
摸清家底,做好质和量的把控.采取分片分类的方式,明确组织、人社、科技、经信和统计5家牵头单位,分医药化工、船舶制造、金属冶炼、木材加工、酿酒食品等五大类,对全县141家规模企业进行全覆盖式的调查摸底.
第三篇: 自然资源人才强国交流材料
人才工作经验交流材料
人才工作经验交流材料
人才工作经验交流材料
新形势下，创新党管人才工作机制，需要赋予其时代特色，更需要结合落实“四个全面”明确其重要抓手和实践形式。党管人才工作的改进和完善可以从以下几个方面着手。
强化组织部门协调的有效性
切实发挥人才工作领导小组作用。建立正常的人才工作领导小组决策机制，确保领导小组发挥应有的议事决策作用。人才工作领导小组会议应正常化，例如原则上每年不少于两次，交流工作进展情况，研究解决重点难点问题。不能因个别原因（如主要领导繁忙）而持续拖延或取消人才工作领导小组会议。建立完善决策咨询制度，对人才工作重大决定和部署，应多方征询专家意见和建议。
加强人才工作队伍建设。健全人才工作体系，适当加强人才工作部门力量和基层人才工作者人员配置。按照“编制、职责、人员、工作”四到位的要求，建立人才工作专门科室，配备专职人员。积极推进人才工作向街道（镇）、园区、国有企事业单位等基层单位延伸，鼓励和支持设立人才工作机构，确保人才工作力量。依托党校、行政学院等培训资源，为人才工作者提供研修培训，不断提高理论水平和工作能力。
强化组织部门统筹协调的有效性。组织部门在履行牵头抓总职能时，要加强与有关单位、有关领导的沟通，督促各部门切实履行职责，坚决破除部门利益、局部利益对人才工作资源的不合理分割；
进一步明确组织部门与人社部门的职能定位，组织部门主要是“管宏观、管政策、管协调、管服务”，应强化战略性管理，落实好牵头抓总职能。人社部门则应加强综合管理职能，要在构建人才服务体系、推动人才队伍建设等方面发挥职能作用。
凝聚共识，形成合力
增强职能部门之间的协调配合。各级人才工作领导小组应按照同级党委（党组）人才工作部署，及时将年度人才工作要点、重点工作任务分解到各有关部门，明确工作质量和进度要求。各同级部门之间加强协作配合，定期或适时召开人才工作协调推进会议，由组织部门牵头协调，邀请相关部门的领导参会，共同协商重点人才工作的推进，真正形成人才工作合力。
定期召开人才工作研讨会。通过人才工作研讨会、公共平台分享等形式加强信息交流，及时通报人才工作方针政策、重大部署，交流各地各部门人才工作动态及经验做法。
鼓励社会力量广泛参与。以市场化为导向，组织引导社会力量广泛参与人才工作。加强对社会组织、行业协会等的引导和激励，扩大人才工作覆盖面。鼓励和支持各类社会组织创新人才服务方式和服务内容，为人才提供个性化和多样化服务。探索建立人才社团联谊会，由政府、企事业单位、社团、专家、人才代表等组成，开展形式多样的联谊活动。
抓好督促落实
促进人才政策措施的贯彻执行。为避免人才工作中党委同行政的不协调，可以建立“党委统一领导下的党政同责制”，把行政纳入到党管人才体制中来，强调“党政同责”。以此增强行政部门参与人才管理工作的积极性，进一步强化人才工作合力，人才工作的开展就会更加落到实处。
健全督促落实机制。对中央和省（市）委、省（市）政府出台的人才政策和制度的执行情况、人才工作重要部署和重点工程落实情况，各级人才办要进行年度检查与日常督查，加强重点工作跟踪指导和专项督查，检查结果要以适当形式予以通报，促进人才工作各项任务落到实处；
实施人才工作目标考核，把人才工作纳入党委、政府领导班子和党政主要领导干部年度目标考核内容。人才工作专项考核结果，要作为衡量领导班子和主要领导干部工作业绩，以及领导干部调整、使用和奖惩的重要依据，以考核促落实；
重视培育和发挥第三方评估机构的作用，开展人才发展规划及相关人才政策落实情况评估。
加强体制外人才引导与服务
营造人才发展的社会和法制环境。在全社会真正形成尊重人才、尊重知识的良好氛围，给予优秀人才和创新人才更多的关心关注，强调“聚天下英才而用之”。
发挥市场在人才工作中的基础性作用。针对体制外人才，要充分发挥市场作用，鼓励和支持人才中介机构为体制外人才提供多样化服务。发展并规范体制内外人才联谊组织，鼓励定期开展各类人才联谊活动，加强沟通，集聚各方面的人才为经济社会发展出谋划策。鼓励和支持企业、社会组织等成立各种类型的人才发展基金，建立健全政府、社会、用人单位和个人多元投入机制，多渠道吸纳和募集人才发展资金。
逐渐打通体制内外人才流动渠道。要充分认识到消除体制界限是社会发展的必然规律，也是人才工作的大势所趋。积极创造条件，打破身份、体制限制，更大范围、更广视野地吸收优秀人才，特别是体制外人才，在体制内外架起一座人才流动的桥梁，使人才可以在体制内外“流得动”。
建立人才分类管理服务机制
尊重行业差别和人才成长规律。探索和总结不同类别人才的成长规律，如区别对待自然科学领域和社会科学领域的人才，对两种类型人才的成长规律分别进行总结；
对于基础研究型和应用实践型人才的考核要各有侧重。人才政策不能“一刀切”，要在科研考核和职称评定等方面为“偏才”留出空间，打通快速成长的通道，提升人才政策的弹性和适应性。
建立区域化人才工作机制。人才工作要有区域化差异，尤其对于经济薄弱、人才匮乏的地区，制定和完善相关扶持政策。建立优秀人才服务偏远地区相关机制，鼓励、激励优秀人才服务、扎根偏远地区，在帮助培养带动一批人才的同时，促进偏远地区经济和社会公共事业的发展。
依托网络互联，加强平台建设
建立人才工作管理平台。由省（市）人才工作协调小组办公室牵头，梳理各部门、各区县相关人才计划和人才政策，在省（市）层面建立人才工作管理平台。将人才服务的信息发布、意见征询与动态监管相结合，提供信息管理、检索、推送、反馈与咨询等服务，实现政策信息与人才信息的区域共享。
搭建人才工作交流联络群。依托微信、微博等即时通讯工具，创新人才工作中的信息发布、即时互动、咨询反馈等服务模式，充分调动广大人才参与交流的积极性和主动性。促进政府部门、人才工作者与人才之间的交流，建设“网上统一战线”。
建立人才联络员制度。按照不同类别或区域设置联络员，加强同各类型人才的联系。人才联络员需要了解相关人才政策信息，为人才提供政策制度咨询和服务，确保各类型人才在需要时能“找到组织”。
第四篇: 自然资源人才强国交流材料
Geography of the United KingdomFrom Wikipedia, the free encyclopedia
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The United Kingdom occupies a substantial part of the British Isles.
The United Kingdom of Great Britain and Northern Ireland, or UK, is a sovereign state located off the northwestern coast of continental Europe. With a total area of approximately 243,610 square kilometres (94,060 sq mi), the UK occupies the major part of the British Isles[1] archipelago and includes the island of Great Britain, the north-eastern one-sixth of the island of Ireland and many smaller surrounding islands. The mainland areas lie between latitudes 49°N and 59°N (the Shetland Islands reach to nearly 61°N), and longitudes 8°W to 2°E. The Royal Greenwich Observatory, in South East London, is the defining point of the Prime Meridian.
The UK lies between the North Atlantic and the North Sea, and comes within 35 km (22 mi) of the northwest coast of France, from which it is separated by the English Channel. It shares a 360 km international land boundary with the Republic of Ireland. The Channel Tunnel bored beneath the English Channel, now links the UK with France.
The British Overseas Territories and Crown Dependencies are covered in their own respective articles, see below.
Content是∙1 Area
∙2 Physical geography
o2.1 Geology
o2.2 Mountains and hills
o2.3 Rivers and lakes
o2.4 Artificial waterways
o2.5 Coastline
▪2.5.1 Inlets
▪2.5.2 Headlands
o2.6 Islands
o2.7 Climate
∙3 Human geography
o3.1 Demographics
o3.2 Political geography
▪3.2.1 National government
▪3.2.2 Local government
o3.3 Economic geography
▪3.3.1 Primary industry
▪3.3.2 Manufacturing
▪3.3.3 Finance and services
▪3.3.4 Regional disparity
∙4 Natural resources
∙5 Environment
o5.1 Current issues
o5.2 International agreements
∙6 Antipodes
∙7 Geography of dependencies
o7.1 Crown dependencies
o7.2 Overseas territories
∙8 See also
∙9 References
∙10 External links
AreaThe total area of the United Kingdom is approximately 245,000 square kilometres (94,600 sq mi), comprising the island of Great Britain, the northeastern one-sixth of the island of Ireland (Northern Ireland) and many smaller islands. England is the largest country of the United Kingdom, at 130,410 square kilometres (50,350 sq mi) accounting for just over half the total area of the UK. Scotland at 78,772 square kilometres (30,410 sq mi),[2] is second largest, accounting for about a third of the area of the UK. Wales and Northern Ireland are much smaller, covering 20,758 square kilometres (8,010 sq mi) and 14,160 square kilometres (5,470 sq mi) respectively.
The area of the countries of the United Kingdom is set out in the table below. Information about the area of England, the largest country, is also broken down by region.
Rank
Name
Area
1
England
130,427 km²
– South West [3]
– East of England
– South East [4]
– East Midlands
– Yorkshire and the Humber
– North West [5]
– West Midlands [6]
– North East [7]
– London [8]
23,837 km²
19,120 km²
19,096 km²
15,627 km²
15,420 km²
14,165 km²
12,998 km²
8,592 km²
1,572 km²
2
Scotland [9]
78,772 km²
3
Wales [10]
20,778 km²
4
Northern Ireland
13,843 km²
United Kingdom
243,820 km²
Overseas territories
1,727,570 km²
The British Antarctic Territory, which covers an area of 1,709,400 km2 is geographically the largest of the British Overseas Territories followed by the Falkland Islands which covers an area of 12,173 km2. The remaining twelve overseas territories cover an area 5,997 km2.
Physical geographyUK"s topography
The physical geography of the UK varies greatly. England consists of mostly lowland terrain, with upland or mountainous terrain only found north-west of the Tees-Exe line. The upland areas include the Lake District, the Pennines, Exmoor and Dartmoor. The lowland areas are typically traversed by ranges of low hills, frequently composed of chalk. The physical geography of Scotland is distinguished by the Highland Boundary Fault which traverses the Scottish mainland from Helensburgh to Stonehaven. The faultline separates the two distinctively different regions of the Highlands to the north and west, and the lowlands to the south and east. Wales is mostly mountainous, though south Wales is less mountainous than north and mid Wales. The geography of Ireland includes the Mourne Mountains as well as Lough Neagh, at 388 square kilometres (150 sq mi), the largest body of water in the UK and Ireland.[11]
The overall geomorphology of the UK was shaped by the combined forces of tectonics and climate change, in particular glaciation.
The exact centre of the island of Great Britain is disputed. Depending upon how it is calculated it can be either Haltwhistle in Northumberland, or Dunsop Bridge in Lancashire.
Geology
See also: Geology of Great Britain and Geology of Ireland
The geology of the UK is complex and diverse, a result of it being subject to a variety of plate tectonic processes over a very extended period of time. Changing latitude and sea levels have been important factors in the nature of sedimentary sequences, whilst successive continental collisions have affected its geological structure with major faulting and folding being a legacy of each orogeny (mountain-building period), often associated with volcanic activity and the metamorphism of existing rock sequences. As a result of this eventful geological history, the UK shows a rich variety of landscapes.[12]
The oldest rocks in the British Isles are the Lewisian gneisses, metamorphic rocks found in the far north west of Scotland and in the Hebrides (with a few small outcrops elsewhere), which date from at least 2,700 Ma (Ma = million years ago). South of the gneisses are a complex mixture of rocks forming the North West Highlands and Grampian Highlands in Scotland. These are essentially the remains of folded sedimentary rocks that were deposited between 1,000 Ma and 670 Ma over the gneiss on what was then the floor of the Iapetus Ocean.
At 520 Ma, what is now Great Britain was split between two continents; the north of Scotland was located on the continent of Laurentia at about 20° south of the equator, while the rest of the country was on the continent of Gondwana near the Antarctic Circle. In Gondwana, England and Wales were largely submerged under a shallow sea studded with volcanic islands. The remains of these islands underlie much of central England with small outcrops visible in many places.
About 500 Ma southern Britain, the east coast of North America and south-east Newfoundland broke away from Gondwana to form the continent of Avalonia, which by 440 Ma had drifted to about 30° south. During this period north Wales was subject to volcanic activity. The remains of these volcanoes are still visible, one example of which is Rhobell Fawr dating from 510 Ma. Large quantities of volcanic lava and ash known as the Borrowdale Volcanics covered the Lake District and this can still be seen in the form of mountains such as Helvellyn and Scafell Pike.
Between 425 and 400 Ma Avalonia had joined with the continent of Baltica, and the combined landmass collided with Laurentia at about 20° south, joining the southern and northern halves of Great Britain together. The resulting Caledonian Orogeny produced an Alpine-style mountain range in much of north and west Britain.
The collision between continents continued during the Devonian period, producing uplift and subsequent erosion, resulting in the deposition of numerous sedimentary rock layers in lowlands and seas. The Old Red Sandstone found in Devon originated from these processes.
Around 360 Ma Great Britain was lying at the equator, covered by the warm shallow waters of the Rheic Ocean, during which time the Carboniferous Limestone was deposited, as found in the Mendip Hills and the Peak District of Derbyshire. Later, river deltas formed and the sediments deposited were colonised by swamps and rain forest. It was in this environment that the Coal Measures were formed, the source of the majority of Britain"s extensive coal reserves.
Around 280 Ma the Variscan orogeny mountain-building period occurred, again due to collision of continental plates, causing major deformation in south west England. The general region of Variscan folding was south of an east–west line roughly from south Pembrokeshire to Kent. Towards the end of this period granite was formed beneath the overlying rocks of Devon and Cornwall, now exposed at Dartmoor and Bodmin Moor.
By the end of the Carboniferous period the various continents of the Earth had fused to form the super-continent of Pangaea. Britain was located in the interior of Pangea where it was subject to a hot arid desert climate with frequent flash floods leaving deposits that formed beds of red sedimentary rock.
As Pangaea drifted during the Triassic, Great Britain moved away from the equator until it was between 20° and 30° north. The remnants of the Variscan uplands in France to the south were eroded down, resulting in layers of the New Red Sandstone being deposited across central England.
Pangaea began to break up at the start of the Jurassic period. Sea levels rose and Britain and Ireland drifted on the Eurasian Plate to between 30° and 40° north. Much of the British Isles were under water again, and sedimentary rocks were deposited and can now be found underlying much of England from the Cleveland Hills of Yorkshire to the Jurassic Coast in Dorset. These include sandstones, greensands, oolitic limestone of the Cotswold Hills, corallian limestone of the Vale of White Horse and the Isle of Portland. The burial of algae and bacteria below the mud of the sea floor during this time resulted in the formation of North Sea oil and natural gas
The modern continents having formed, the Cretaceous saw the formation of the Atlantic Ocean, gradually separating northern Scotland from North America. The land underwent a series of uplifts to form a fertile plain. After 20 million years or so, the seas started to flood the land again until much of Britain and Ireland were again below the sea, though sea levels frequently changed. Chalk and flints were deposited over much of Great Britain, now notably exposed at the White Cliffs of Dover and the Seven Sisters, and also forming Salisbury Plain.
Between 63 and 52 Ma, the last volcanic rocks in Great Britain were formed. The major eruptions at this time produced the Antrim Plateau, the basaltic columns of the Giant"s Causeway and Lundy Island in the Bristol Channel.
The Alpine Orogeny that took place in Europe about 50 Ma, was responsible for the folding of strata in southern England, producing the London Basin syncline, the Weald-Artois Anticline to the south, the North Downs, South Downs and Chiltern Hills.
During the period the North Sea formed, Britain was uplifted. Some of this uplift was along old lines of weakness left from the Caledonian and Variscan Orogenies long before. The uplifted areas were then eroded, and further sediments, such as the London Clay, were deposited over southern England.
The major changes during the last 2 million years were brought about by several recent ice ages. The most severe was the Anglian Glaciation, with ice up to 1,000 m (3300 ft) thick that reached as far south as London and Bristol. This took place between about 478,000 to 424,000 years ago, and was responsible for the diversion of the River Thames onto its present course. During the most recent Devensian glaciation, which ended a mere 10,000 years ago, the icesheet reached south to Wolverhampton and Cardiff. Among the features left behind by the ice are the fjords of the west coast of Scotland, the U-shaped valleys of the Lake District and erratics (blocks of rock) that have been transported from the Oslo region of Norway and deposited on the coast of Yorkshire.
Amongst the most significant geological features created during the last twelve thousand years are the peat deposits of Ireland and Scotland, and of coastal and upland areas of England and Wales.
At the present time Scotland is continuing to rise as a result of the weight of Devensian ice being lifted. Southern and eastern England is sinking, generally estimated at 1 mm (1/25 inch) per year, with the London area sinking at double the speed partly due to the continuing compaction of the recent clay deposits.
Mountains and hills
At 1,344 metres, Ben Nevis is the highest peak in the UK.
Main article: List of mountains and hills of the United Kingdom
The ten tallest mountains in the UK are all found in Scotland. The highest peaks in each part of the UK are:
∙Scotland: Ben Nevis, 1,344 metres
∙Wales: Snowdon (Snowdonia), 1,085 metres
∙England: Scafell Pike (Cumbrian Mountains), 978 metres
∙Northern Ireland: Slieve Donard (Mourne Mountains), 852 metres
The ranges of mountains and hills in the UK include:
∙Scotland: Cairngorms, Scottish Highlands, Southern Uplands, Grampian Mountains
∙Wales: Brecon Beacons, Cambrian Mountains, Snowdonia, Black Mountains, Preseli Hills
∙England: Cheviot Hills, Chilterns, Cotswolds, Dartmoor, Lincolnshire Wolds, Exmoor, Lake District, Malvern Hills, Mendip Hills, North Downs, Peak District, Pennines, South Downs, Shropshire Hills, Yorkshire Wolds
∙Northern Ireland: Mourne Mountains, Antrim Plateau, Sperrin Mountains
The lowest point of the UK is in the Fens of East Anglia, in England, parts of which lie up to 4 metres below sea level.
Rivers and lakes
Main articles
∙List of lakes and lochs in the United Kingdom;
∙List of rivers of the United Kingdom;
∙List of waterfalls of the United Kingdom.
The longest river in the UK is the River Severn (220 mi, 354 km) which flows through both Wales and England.
The longest rivers in the UK contained wholly within each of its constituent nations are:
∙England: River Thames (215 mi, 346 km)
∙Scotland: River Tay (117 mi, 188 km)
∙N. Ireland: River Bann (76 mi, 122 km)
∙Wales: River Tywi (64 mi, 103 km)
The largest lakes (by surface area) in the UK by country are:
∙N. Ireland: Lough Neagh (147.39 sq mi, 381.74 km²)
∙Scotland: Loch Lomond (27.46 sq mi, 71.12 km²)
∙England: Windermere (5.69 sq mi, 14.74 km²)
∙Wales: Llyn Tegid (Bala Lake) (1.87 sq mi, 4.84 km²)
The deepest lake in the UK is Loch Morar with a maximum depth of 309 metres (Loch Ness is second at 228 metres deep). The deepest lake in England is Wastwater which achieves a depth of 79 metres (258 feet).
Artificial waterways
Main articles: Waterways in the United Kingdom, Canals of Great Britain, Reservoirs and dams in the United Kingdom
As a result of its industrial history, the United Kingdom has an extensive system of canals, mostly built in the early years of the Industrial Revolution, before the rise of competition from the railways. The United Kingdom also has numerous dams and reservoirs to store water for drinking and industry. The generation of hydroelectric power is rather limited, supplying less than 2% of British electricity mainly from the Scottish Highlands.
Coastline
United Kingdom maritime claims
The UK has a coastline which measures about 12,429 km[citation needed]. The heavy indentation of the coastline helps to ensure that no location is more than 125 km from tidal waters.
The UK claims jurisdiction over the continental shelf, as defined in continental shelf orders or in accordance with agreed upon boundaries, an exclusive fishing zone of 200 nmi (370.4 km; 230.2 mi), and territorial sea of 12 nmi (22.2 km; 13.8 mi).
Inlets∙Cardigan Bay
∙Lyme Bay
∙Bristol Channel
∙Thames estuary
∙Morecambe Bay
∙Solway Firth
∙The Wash
∙Humber estuary
∙Firth of Forth
∙Firth of Tay
∙Moray Firth
HeadlandsThe geology of the United Kingdom is such that there are many headlands along its coast. A list of headlands of the United Kingdom details many of them.
Islands
See main list of islands of the United Kingdom
In total, it is estimated that the UK is made up of over one thousand small islands, the majority located off the north and west coasts of Scotland.
Climate
Main article: Climate of the United Kingdom
The climate of the UK is generally temperate, although significant local variation occurs, particularly as a result of altitude and distance from the coast. In general the south of the country is warmer than the north, and the west wetter than the east. Due to the warming influence of the Gulf Stream, the UK is significantly warmer than some other locations at similar latitude, such as Newfoundland.
The prevailing winds are southwesterly, from the North Atlantic Current. More than 50% of the days are overcast.[citation needed] There are few natural hazards, although there can be strong winds and floods, especially in winter.
Average annual rainfall varies from over 3,000 mm (118.1 in) in the Scottish Highlands down to 553 mm (21.8 in) in Cambridge. The county of Essex is one of the driest in the UK, with an average annual rainfall of around 600 mm (23.6 in), although it typically rains on over 100 days per year. In some years rainfall in Essex can be below 450 mm (17.7 in), less than the average annual rainfall in Jerusalem and Beirut.
The highest temperature recorded in the UK was 38.5 °C (101.3 °F) at Brogdale, near Faversham, in the county of Kent, on 10 August 2003. The lowest was −27.2 °C (−17.0 °F) recorded at Braemar in the Grampian Mountains, Scotland, on 11 February 1895 and 10 January 1982 and Altnaharra, also in Scotland, on 30 December 1995.
Human geographyThe United Kingdom is composed of four parts: England, Northern Ireland, Scotland and Wales.
The United Kingdom"s cities, other large centres, and selected smaller places
Demographics
Main article: Demographics of the United Kingdom
Political geography
Main article: Politics of the United Kingdom
National governmentThe UK is governed as a whole by the Parliament of the United Kingdom. Of the four countries that make the UK, Scotland, Wales and Northern Ireland have devolved administrations and parliaments/assembly:
∙Northern Ireland – Northern Ireland Assembly
∙Scotland – Scottish Parliament
∙Wales – National Assembly for Wales
England has no devolved system of government[clarification needed]that is, the Parliament of the United Kingdom serves as (and historically was) the English Parliament. It is governed by UK government ministers and legislated for by the UK parliament. Within England, London has a devolved assembly but proposals for elected Regional Assemblies in England were rejected in the first referendum covering North East England. See Government of England.
The UK (specifically, Northern Ireland) has an international land boundary with the Republic of Ireland of 360 km. There is also a boundary between the jurisdiction of France and the UK on the Channel Tunnel.
Local governmentMain articles: Local government in England, Local government in Scotland, Local government in Wales, and Local government in Northern Ireland
Each part of the UK is subdivided in further local governmental regions:
∙England: Unitary Authorities, county councils, district councils, parish councils
∙Wales: Principal areas, communities
∙Scotland: Council areas, communities
∙Northern Ireland: Districts
Historically the UK was divided into counties or shires: administrative areas through which all civil responsibilities of the government were passed. Each county or shire had a county town as its administrative centre and was divided into individual parishes that were defined along ecclesiastic boundaries.
Between 1889 (1890 in Scotland) and 1974, the political boundaries were based on the traditional counties, but due to changes in population centres, the traditional counties became impractical as local government areas in certain highly urbanised areas. The Local Government Act 1972 created a new system of administrative counties, designed to take account of the widely differing populations across different parts of the country.
In the 1990s further population growth led to more political changes on a local level. Unitary authorities were formed across the entire of Scotland and Wales, and in larger cities in England. Many unpopular administrative counties were also abolished at this time, leading to a mixture of two-tier and single-purpose authorities. Further reorganisations are planned if and when regional assemblies in England are revisited in the future.
Economic geography
Main article: Economic geography of the United Kingdom
The economic geography of the UK reflects not only its current position in the global economy, but its long history both as a trading nation and an imperial power.
The UK led the industrial revolution and its highly urban character is a legacy of this, with all its major cities being current or former centres of various forms of manufacturing. However, this in turn was built on its exploitation of natural resources, especially coal and iron ore.
Primary industryThe UK"s primary industry was once dominated by the coal industry, heavily concentrated in the north, the Midlands and south Wales. This is all but gone and the major primary industry is North Sea oil. Its activity is concentrated on the UK Continental Shelf to the north-east of Scotland.
ManufacturingThe UK"s heavy manufacturing drove the industrial revolution. A map of the major UK cities gives a good picture of where this activity occurred, in particular Belfast, Birmingham, Glasgow, Liverpool, London, Manchester, Newcastle and Sheffield. Today there is no heavy manufacturing industry in which UK-based firms can be considered world leaders. However, areas of the UK still have a notable manufacturing base, including the Midlands which remains a strong manufacturing centre, and the North West which accounts for 60% of the United Kingdom"s manufacturing output.[13] More recently, high technology firms have concentrated largely along the M4 motorway, partly because of access to Heathrow Airport, but also because of agglomeration economies.
Finance and servicesOnce, every large city had a stock exchange. Now, the UK financial industry is concentrated overwhelmingly in the City of London and Canary Wharf, with back office and administrative operations often dispersed around the south of England. London is one of the world"s great financial centres and is usually referred to as a world city. There is also a significant legal and ebusiness industry in Leeds.
Regional disparityThe effect of changing economic fortune has contributed to the creation of the so-called North-South divide, in which decaying industrial and ex-industrial areas of Northern England, Scotland and Wales contrast with the wealthy, finance and technology-led southern economy. This has led successive governments to develop regional policy to try to rectify the imbalance. However this is not to say that the north-south divide is uniform; some of the worst pockets of deprivation can be found in London, whilst parts of Cheshire and North Yorkshire are very wealthy. Nor is the North-South divide limited to the economic sphere; cultural and political divisions weigh heavily too.
Natural resourcesMain article: Economy of the United Kingdom
Historically, much of the United Kingdom was forested. Since prehistoric times, man has deforested much of the United Kingdom.
Agriculture is intensive, highly mechanised, and efficient by European standards, producing about 60% of food needs with only 1% of the labour force. It contributes around 2% of GDP. Around two thirds of production is devoted to livestock, one third to arable crops.
In 1993, it was estimated that land use was:
∙Arable land: 25%
∙Permanent crops: 0%
∙Permanent pastures: 46%
∙Forests and Woodland: 10%
∙Other: 19%
∙Irrigated: 1,080 km²
The UK has a variety of natural resources including:
∙Geological: coal, petroleum, natural gas, limestone, chalk, gypsum, silica, rock salt, china clay, iron ore, tin, silver, gold, lead.
∙Agricultural: arable land, wheat, barley, sheep
The UK has large coal, natural gas, and oil reserves; primary energy production accounts for 10% of GDP, one of the highest shares of any industrial nation. Due to the island location of the UK, the country has great potential for generating electricity from wave power and tidal power, although these have not yet been exploited on a commercial basis.
EnvironmentCurrent issuesEngland is one of the most densely populated countries/regions in the world, and the most densely populated major nation in Europe.[14] The high population density (especially in the southeast of England) coupled with a changing climate, is likely to put extreme pressure on the United Kingdom"s water resources in the future.[15]
The United Kingdom is reducing greenhouse gas emissions. It has met Kyoto Protocol target of a 12.5% reduction from 1990 levels and intends to meet the legally binding target of a 20% cut in emissions by 2010. By 2015, to recycle or compost at least 33% of household waste. Between 1998-99 and 1999–2000, household recycling increased from 8.8% to 10.3% respectively.
International agreements
The United Kingdom is a party to many international agreements, including: Air Pollution, Air Pollution-Nitrogen Oxides, Air Pollution-Sulphur 94, Air Pollution-Volatile Organic Compounds, Antarctic-Environmental Protocol, Antarctic-Marine Living Resources, Antarctic Seals, Antarctic Treaty, Biodiversity, Climate Change, Climate Change-Kyoto Protocol, Desertification, Endangered Species, Environmental Modification, Hazardous Wastes, Law of the Sea, Marine Dumping, Marine Life Conservation, Nuclear Test Ban, Ozone Layer Protection, Ship Pollution, Tropical Timber 83, Tropical Timber 94, Wetlands and Whaling.
The UK has signed, but not ratified, the international agreement on Air Pollution-Persistent Organic Pollutants.
AntipodesThe antipodes of the British Isles lie in the South Pacific, between New Zealand"s Campbell Islands (off southern Ireland) and Antipodes Islands (across the Channel in Normandy). However, several British Overseas Territories are antipodal to land.
The antipodes of the Falkland Islands overlie the border of Chinese northern Inner Mongolia and Russian Siberia (Trans-Baikal Territory). Neighboring uninhabited South Georgia Island equates to the northern tip of Sakhalin. The southern South Sandwich Islands overlap with Russia near Magadan.
Gibraltar just touches the coast of New Zealand between Auckland and Whangarei. The Pitcairns are in Saudi Arabia, near the coast with Qatar and Bahrain, while neighboring Ducie"s are in the UAE between Dubai and Abu Dhabi. Bermuda isn"t antipodal to land, but is close, within 30 km of the Australian coast near Perth.
第五篇: 自然资源人才强国交流材料
封 面作者：ZHANGJIAN
仅供个人学习，勿做商业用途
人力资源经验交流发言材料
各位领导、同事大家好！
古人云：得人者得天下，失人者失天下。在当今市场竞争日趋激烈的环境下，人才的竞争尤为突出，因此人力资源的开发与管理成为企业发展的重要工作之一。可以说，企业的生存与发展，关键在于人才。如何正确理解现代人力资源管理理念，如何运用有效的管理机制引入人才、留住人才，如何将现有的人力资源充分开发利用，如何发掘员工的潜能及主观能动性，为企业的发展尽心尽力努力工作，减少人才的流失，是我们需要关注的一个重要课题。个人收集整理 勿做商业用途
结合这样一个课题,先同大家分享一个人力资源管理学中的一个经典案例:
B公司是一家日化产品生产企业。几年来，公司业务一直发展很好，销售量逐年上升。B公司在办公室下设立了一个人事主管，从事员工的考勤、招聘、档案管理等人事管理。每到销售旺季，公司就会让人事主管到人才市场大批招聘销售人员，一旦到了销售淡季，公司又会大量裁减销售人员。公司在丢失打印机后会专门成立调查小组进行调查，而对公司个别骨干的跳槽却不闻不问。对此公司销售经理曾给总经理提过几次意见。而总经理却说：“人才市场中有的是人。只要我们工资待遇高，还怕找不到人吗?一年四季把他们‘养’起来，费用太大。”这样，B公司的销售人员流动性很大，连销售骨干也开始纷纷跳槽。总经理对销售骨干极力挽留，但没有效果，只能重新招聘。个人收集整理 勿做商业用途
某年，正值公司销售旺季之际，跟随总经理多年的销售经理和公司大部分销售人员集体辞职。致使公司销售工作一时近乎瘫痪。这时，总经理才感到问题有些严重。因为人才市场上可以招到一般的销售人员，但不一定总能找到优秀的销售人才和管理人才。在这种情况下，他亲自到销售经理家中，开出极具诱惑力的年薪，希望他和一些销售骨干能重回B公司，但依然没能召回这批老部下。这时总经理才有些后悔，为什么以前没有下工夫去留住这些人才呢?同时他陷入了困惑， 如此高薪，他们为什么也会拒绝。企业到底靠什么留住人才呢?类似这样的案例在现代企业中并不是个别现象。在新环境下，有很多优秀的技术人才和管理人才放弃了高薪，放弃了名利，离开了原来的工作岗位而另觅他处。是什么让他们置丰厚的薪酬于不顾？难道还有什么东西比高薪更能吸引人才，能留住人才的么?个人收集整理 勿做商业用途
在解决这个问题之前，先分析一下B公司在人力资源管理方面存在的问题。
首先，B公司缺乏正确的人力资源观。B公司的管理是传统的以“事”为中心。而不是以“人”为中心的管理。这一点，可以从公司组织结构中看出，B公司只设一个人事主管，职能只是一些简单的人事管理。此外，对于丢失打印机成立了专门小组去调查追究，而对个别骨干员工的跳槽却置之不理，这也表现出该公司没有充分树立“以人为本”的现代管理理念。个人收集整理 勿做商业用途
其次，B公司内部各部门之间缺少沟通。总经理与其员工之间的交流尤其需要增多，总经理对于他人的意见应该给与慎重的考虑和斟酌，不应该草率的下定论。例如销售经理给总经理提意见却不子考虑等方面，可以体现出公司在各部门广泛沟通和交流方面还有待改善和加强。个人收集整理 勿做商业用途
再次，B公司在对员工的招聘、培训，个人发展和职业规划等方面也存在一些弊端。公司在招聘人才的时候采用的是旺季大批招聘、淡季大批裁员的机制，使其在招聘环节处于被动。而且缺少了培训的环节。使员工上岗后不适应工作环境，缺少自信心和安全水平。此外，由于人员流动性大的特点，公司毫不考虑员工的个人发展和素质提高。也不会督促和提醒员工制定自己的职业生涯规划，这一点对员工自身和公司业绩都是非常不利的。个人收集整理 勿做商业用途
最后，B公司没有健全的激励机制和良好的企业文化。虽说物质需要始终是人类的第一需要，薪水是员工考虑的第一要素，但是物质满足并不能代表员工们所要的一切。现在的社会中，人们越来越讲究精神满足和心理满足。正如案例中所述， 当总经理向他的老部下提供丰个人收集整理 勿做商业用途
厚的薪水时，老部下并没有继续任职。由此可见，心理层面和精神层面的需要已经重于物质层面的需要。这就要求企业建立健全激励机制，既有物质激励，更要有精神激励。同时注重企业文化的培养，创建一个舒适、和谐的工作环境，让员工在企业中找到归属感和成就感，充分彰显“以人为本”的人性化企业文化。个人收集整理 勿做商业用途
综合以上原因，我们不难发现。公司之所以留不住人才是综合了多方面因素的，除了薪酬福利等必要的物质基础，更重要的是公司没有真正建立现代的人力资源观和管理理念，不重视人才的培养和发展，领导缺乏个人魅力等等。个人收集整理 勿做商业用途
那么，面对如何吸收人才，留住人才的问题，我想结合我所学到的人力资源管理知识，着重谈一下如何留住人才的方法和对策。个人收集整理 勿做商业用途
一、树立现代人力资源管理理念，完善企业内部管理
人力资源管理主要研究如何最有效、最合理地管理和使用企业所拥有的最宝贵的资源— — 员工们的才能与热情。从而实现企业的既定目标，使其经济效益和社会效益最大化。随着当代社会经济的发展，人力资源管理因其与人的关系密切而变得日益重要。随着市场竞争的加剧，管理领域的扩大，人力资源管理的重要性更加凸显。它对组织目标的实现，提高员工的工作绩效，增强组织竞争力等方面具有重要意义。个人收集整理 勿做商业用途
现代人力资源管理更注重人本原理，增加了很多新措施。例如改善奖酬福利、工作条件、提供个人发展机会、完善激励制度、发展民主参与和管理等等。这些新措施都是为了改善员工全面工作、生活质量，提高其工作满意感，增强他们组织归属感。除此之外，现代管理注重招聘，组织员工上岗前培训，协调各部门组织绩效考评，培养良好的企业文化氛围。以上措施都是围绕“以人为本”的管理理念的树立而展开的。目的在于完善企业内部管理，这是留住人才的的重要因素。个人收集整理 勿做商业用途
二、立足长远，注重员工的招聘和培训
招聘是为了企业发展的需要和要求，通过信息的发布和科学甄选，获得本企业所需的合格人才，并安排他们到企业所需岗位工作的活动和过程。它是人力资源管理中的一个非常重要的环节，是人才进入企业的第一关。企业只有对招聘环节进行有效的设计和良好的管理，才能以较低的招聘成本获得高质量的员工，从立足长远的角度来看，招聘到优秀的人才是企业发展进步的力量源泉，像上文B公司那样对招聘不重视的做法是很不妥当的。培训作为现代企业管理的重要内容和手段，已越来越被企业所重视。企业培训主要体现在三个方面，即知识的学习，技能的提高，态度的转变。培训的目的主要有四项：育道德、建观点、传知识、培能力，缺一不可。具体地说，一方面，通过培训，可以改变员工的工作态度，增长知识，提高技能，激发他们的创造力和潜能，提高企业运作效率和销售业绩。使企业直接受益；
另一方面，也增强员工自身的素质和能力，让员工认识到培训是公司为他们提供的最好福利，是公司给他们的最好礼物。同时，从公司未来发展的角度看，教育和培训跟上了。人才就具有了连续性，而且凝聚力也会大大加强。个人收集整理 勿做商业用途
三、提供人才发展空间，帮助员工构建职业生涯规划
当代社会追求自身价值实现的员工越来越多，发展空间和成长机会成为他们选择企业的重要标准之一。企业为优秀人才提供成长与发展空间，保证其自身的不断提高，可以帮助人才充分发挥和利用其潜能，更大程度地实现自身价值。同时会令他们感受到个人职业发展的前景乐观，从而增强对企业的归属感和责任感，自觉地留在企业，竭力为企业服务。因此，企业要留住人才就必须努力为员工提供成长与发展的空间。这就要求企业树立长远发展目标。并帮助员工构建与企业发展目标紧密联系的职业生涯规划，使员工能够清楚自己所处的位个人收集整理 勿做商业用途
置，了解与企业一起成长发展的机会。企业同时也要制定详细明确的发展战略、发展规划。为员工创造良好的就业发展环境，“天高任鸟飞，海阔凭鱼跃”。只有把企业发展和员工命运紧紧相连才是留住人才的法宝。个人收集整理 勿做商业用途
四、加强企业内部沟通
良好的沟通可以及时了解员工的思想动态和相关信息，减少他们对企业的不满，改进企业在人才管理上的缺陷，从而减少人才流失。可以说，会用、用好具有不同特色的人才是一门管理上的艺术。通过在公司内定期举办讨论、交流会等措施。让员工与管理者全面、坦诚地进行双向沟通。同时，公司可以设立意见箱，鼓励员工多提意见和建议，并对切实可行的意见予以奖励。这样，使领导与员工之间不再只是一种单纯的领导与被领导关系，而是一种全新的伙伴式关系，共个人收集整理 勿做商业用途
同营造出一种民主、进取、合作的健康氛围。企业同时要重视员工之间人际关系的改善，企业中人际关系的改善不仅有助于企业效益的提高。还可以增强企业的凝聚力，展示出团结进取的精神面貌，进而留住人才。个人收集整理 勿做商业用途
五、建立健全有效的激励制度
激励对管理，特别是对人力资源管理的重要性自不待言。它不仅在于使员工安心积极的工作，还在于能使员工认同和接受本企业的目标与价值观，对企业产生强烈归属感的作用。如果能激发起员工的干劲，使他们乐于为企业工作，那么留住人才的目的也就达到了。谈到激励，许多企业自然就会想到用高薪留住人才。的确，高薪是能吸引人，但不一定能留住人，而精神的激励— — 成就感、认同感才是留住人才的重要因素。但这一点却往往被许多企业所忽视。行为科学家赫兹伯格的双因素理论就认为，工资、工作条件、工作环境等属于“保健”因素，它不具有激励作用，而工作成就、社会认可、发展前途等因素才是真正的激励因素。因此，举办经验交流会，让公司中优秀的员工将他们的经验与大家共享，让大家都来认可他们的工作成就；
为优秀的员工提供合理及时的晋升机会，推行参与式管理，培养员工的主人翁意识等，都是值得推行的激励措施。个人收集整理 勿做商业用途
六、培养健康和谐的企业文化
企业文化是企业在长期生产经营活动中所形成的全体员工共同认可的价值规范。优秀的企业文化对员工有很好的激励、约束和凝聚作用。它可以把职工和企业紧紧联系在一起，带动员工树立明确的目标。并在为此目标奋斗的过程中与企业保持一致的步调，使每个员工产个人收集整理 勿做商业用途
生归属感和荣誉感。共同的价值观，共同的信念会使员工凝聚成一个整体，增强企业的凝聚力和向心力，这才是企业发展的核心竞争力。所以，塑造优秀企业文化也是留住人才的重要措施之一。个人收集整理 勿做商业用途
综上所述，要留住人才，高薪高待遇并不是唯一途径。我们可以从人力资源管理的角度出发，多层次分析员工的物质需求和精神需求。在管理层的支持下进行现代科学管理制度的建设。加强内部沟通交流，为员工提供发展空间和机会，创建和谐向上的企业文化，这才是企业留住人才的真经之所在。个人收集整理 勿做商业用途
谢谢大家！我的发言完毕。
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