成都理工大学：《环境地质学》课程PPT教学课件（双语讲稿）第一讲 环境地质学概念及学习意义（主讲人：万新南）

环境地质学概念及学习意义 Concept of Environmental geology 1、环境地质学概念( Concept) 是认识“系统环境”的一门综合性学科, 是研究环境科学、地质科学,系统了解地球本身的一门基础科学。 人类只有一个地球,共同的家园。 2、环境地质学学习意义( why study it) 不了解地球的学者不算一个完美的学者,环境地学知识能使其它 学科,在设计施工、决策上站在“地球环境”的高度上考虑问题。 3、授课对象( who study it) 主要针对非地学类专业(文科、非地学的理科、如农业、电子、医 也可针对地学类学生 环质 Environmental Geology

环境地质学 Environmental Geology 环境地质学概念及学习意义 Concept of Environmental geology 1、环境地质学概念(Concept) •是认识“系统环境”的一门综合性学科， •是研究环境科学、地质科学，系统了解地球本身的一门基础科学。 人类只有一个地球，共同的家园。 2、环境地质学学习意义(why study it) 不了解地球的学者不算一个完美的学者，环境地学知识能使其它 学科，在设计施工、决策上站在“地球环境”的高度上考虑问题。 3、授课对象（who study it) 主要针对非地学类专业(文科、非地学的理科、如农业、电子、医 学，环境工程等），也可针对地学类学生

视实中的圆与境 Geology Environment, then and nowe 文明依地质条件的应允而存,但这种条件却元时 不刻地在潜移默化。(可以真实体会学习环境地 质学的真谛) Civilization exists by geological consent subject to change without notice. (Will Durant) ·四川省安县国家地质公园则是现实中的环境一地质一风景 文明溶为一体的典型地区。(观看成都理工大学制作的 地质与文明”的科教片,20分钟—一该片溶汇了“环境 地质学”的大部分内容,是体会该课程的总纲与先导) 环质 Environmental Geology

环境地质学 Environmental Geology 现实中的地质与环境 Geology & Environment, then and now • 文明依地质条件的应允而存，但这种条件却无时 不刻地在潜移默化。（可以真实体会学习环境地 质学的真谛） Civilization exists by geological consent, subject to change without notice.( Will Durant) • 四川省安县国家地质公园则是现实中的环境－地质－风景 －文明溶为一体的典型地区。（观看成都理工大学制作的 “地质与文明”的科教片，20分钟－－该片溶汇了“环境 地质学”的大部分内容，是体会该课程的总纲与先导）

第一部分:宇容与北球 Chapter 1: Our Planetary Environment 星际环境 The Universe Environment 2、时空中的地球 Earth in Space and Time 3、生命演化与人口形势 Biology evolution and Population 4、地球物质的化学组成 Rock and minerals in earth 环质 Environmental Geology

环境地质学 Environmental Geology 第一部分：宇宙与地球 Chapter 1: Our Planetary Environment 1、星际环境The Universe Environment 2、时空中的地球 Earth in Space and Time 3、生命演化与人口形势 Biology evolution and Population 4、地球物质的化学组成 Rock and Minerals in earth

星际邳境 The Planetary environment 1)囵的形成 Our Universe 大爆炸理论:“ Big bang”-发生在150亿年前 In recent decades scientists have been able to construct an ever clearer picture of the origins of the solar system and before that of the universe itself. Most astronomers now accept some sort of Big Bang as origin of today' s universe. at that time enormous quantities of matter were created and flung x ja violently apart across an ever- larger volume of space. The time of Big Bang can be estimated in several ways perhaps the most direct is the back-calculation of the universe's expansion to its apparent beginning. Other methods depend on astrophysical天体物理 models of creation of the elements or the rate of evolution of different types of stars. Most age estimates overlap in the range of 15 to 20 billion years, although a few researchers suggest an age closer to 10 billion years 环质 Environmental Geology

环境地质学 Environmental Geology 1、星际环境 The Planetary Environment 1）宇宙的形成 Our Universe 大爆炸理论：“Big Bang”-发生在150亿年前 In recent decades, scientists have been able to construct an ever￾clearer picture of the origins of the solar system and, before that, of the universe itself. Most astronomers now accept some sort of “Big Bang” as origin of today’s universe. At that time, enormous quantities of matter were created and flung投掷 violently apart across an ever￾larger volume of space. The time of Big Bang can be estimated in several ways. Perhaps the most direct is the back-calculation of the universe’s expansion to its apparent beginning. Other methods depend on astrophysical天体物理 models of creation of the elements or the rate of evolution of different types of stars. Most age estimates overlap in the range of 15 to 20 billion years, although a few researchers suggest an age closer to 10 billion years

T星欧邳境 The Planetary environment 2)彩的形成 Our Universe 大爆炸理论:在重力作用下、碎片聚集、能量释放 From the debris of the Big bang formed the stars, as locally high concentrations of mass were collected together by gravity, and some became large and dense enough that energy-releasing atomic reactions were set off deep within them. Stars are not permanent objects. They are constantly losing energy and mass as they burn their nuclear fuel. The mass of material that initially formed the star determines how rapidly the star burn; some stars burned out billions of years ago, while others are probably forming now from the original matter of the universe mixed with the debris of older stars 环质 Environmental Geology

环境地质学 Environmental Geology 1、星际环境 The Planetary Environment 2）星球的形成 Our Universe 大爆炸理论：在重力作用下、碎片聚集、能量释放 From the debris of the Big Bang formed the stars, as locally high concentrations of mass were collected together by gravity, and some became large and dense enough that energy-releasing atomic reactions were set off deep within them. Stars are not permanent objects. They are constantly losing energy and mass as they burn their nuclear fuel. The mass of material that initially formed the star determines how rapidly the star burn; some stars burned out billions of years ago, while others are probably forming now from the original matter of the universe mixed with the debris of older stars

、星际环境 The Planetary Environment 3)宏贴图的形成 Our Universe 大爆炸理论:高速旋转的、浑沌的星云团开始分异 Our sun and its system of circling planets, including the earth, are believed to have formed from a rotating cloud of gas and dust, starting nearly 5 billion years ago. Most of the mass of the cloud coalesced to form the sun which became a star and began to shine", or release light energy when its interior became so dense and hot from the crushing effects of its own gravity that nuclear reactions were trigged inside it, Meanwhile, dust condensed from the gases remaining in the flattened cloud disk rotating around the young sun. The dust clumped into planets, the formation of which was essentially complete over 4.5 billion years ago 环质 Environmental Geology

环境地质学 Environmental Geology 1、星际环境 The Planetary Environment 3）太阳系的形成 Our Universe 大爆炸理论：高速旋转的、浑沌的星云团开始分异 Our sun and its system of circling planets, including the earth, are believed to have formed from a rotating cloud of gas and dust, starting nearly 5 billion years ago. Most of the mass of the cloud coalesced to form the sun, which became a star and began to “shine”, or release light energy, when its interior became so dense and hot from the crushing effects of its own gravity that nuclear reactions were triggred inside it, Meanwhile, dust condensed from the gases remaining in the flattened cloud disk rotating around the young sun. The dust clumped into planets, the formation of which was essentially complete over 4.5 billion years ago

大爆炸初期所形成的星云团 美国宇航局说,“哈勃”太空望远镜新拍到了迄今有关可见宇宙最纵深景观的照 片,这张具有历史意义的照片中可能包含着宇宙诞生后不久产生的最早期星系。 环质 Environmental Geology

环境地质学 Environmental Geology 大爆炸初期所形成的星云团 美国宇航局说，“哈勃”太空望远镜新拍到了迄今有关可见宇宙最纵深景观的照 片，这张具有历史意义的照片中可能包含着宇宙诞生后不久产生的最早期星系

大爆炸初期所形成的星云团 科学界普遍认为,宇宙诞生于距今约137亿年前的“大爆炸”。在形大爆 后的3亿年中,宇宙处于黑暗和冷寂状态,随后第一批恒星以及星系开始产生 “哈勃”新拍下的照片捕获到的正是宇宙中首批星系所发出的光芒。 环质 Environmental Geology

环境地质学 Environmental Geology 大爆炸初期所形成的星云团 科学界普遍认为，宇宙诞生于距今约１３７亿年前的“大爆炸”。在“大爆炸” 后的３亿年中，宇宙处于黑暗和冷寂状态，随后第一批恒星以及星系开始产生。 “哈勃”新拍下的照片捕获到的正是宇宙中首批星系所发出的光芒

现实容国中的星你 3月4日,美国宇航局公布一张由"哈勃 太空望远镜拍摄的一颗名为"V838 Mon"的恒星及其周围景象的照片。宇 航局称,这张照片与荷兰绘画大师凡 高的名作《星夜》有"异常相似"之处 环质 Environmental Geology

环境地质学 Environmental Geology 现实宇宙中的星体 3月4日，美国宇航局公布一张由"哈勃 "太空望远镜拍摄的一颗名为"V838 Mon"的恒星及其周围景象的照片。宇 航局称，这张照片与荷兰绘画大师凡· 高的名作《星夜》有"异常相似"之处

现实容国中的星你 这是荷兰绘画大师凡高1889年 在法国南部圣雷米精神病院治 疗期间创作的名画《星夜》。 在画中,漩涡状星云扫过夜空 其手法大胆,震撼人心。该 画被视为凡高最具风格的代表 作之 环质 Environmental Geology

环境地质学 Environmental Geology 现实宇宙中的星体 这是荷兰绘画大师凡·高1889年 在法国南部圣雷米精神病院治 疗期间创作的名画《星夜》。 在画中，漩涡状星云扫过夜空 ，其手法大胆，震撼人心。该 画被视为凡·高最具风格的代表 作之一