The document discusses chemical weathering, which is the breakdown of rocks through chemical processes. It occurs when rocks interact with substances like water, oxygen, and carbon dioxide in the atmosphere. There are four main types of chemical weathering: oxidation, solution, carbonation, and biotic weathering. The document provides details on each type of chemical weathering and includes objectives, diagrams, and a quiz for students.
The Soufrière Hills volcano on the island of Montserrat erupted in 1995 due to its location on a destructive plate boundary, where the Atlantic oceanic plate is subducting under the Caribbean continental plate. As magma rose from the subducting plate it formed the composite Soufrière Hills volcano. In June 1997, the volcano's dome collapsed, sending pyroclastic flows down the mountain that engulfed villages, killing 19 people. The eruption destroyed homes and infrastructure across the southern half of the island.
CAMBRIDGE GEOGRAPHY AS EXTRA REVISION - EXAM STYLE QUESTIONS 2 - ATMOSPHERE A...George Dumitrache
Insolation refers to the solar radiation received from the sun, and albedo is the proportion of solar radiation reflected by a surface. Insolation would be greater and albedo lower in a tropical rainforest compared to a polar ice cap due to differences in surface reflectivity. Coastal areas may have higher temperatures than continental areas at the same latitude due to the moderating influence of bodies of water on temperature. Aspect, or the direction a slope faces, can also impact temperature, with sunnier south-facing slopes being warmer than north-facing slopes. The passage also defines dry adiabatic lapse rate and saturated adiabatic lapse rate, and explains how an understanding of lapse rates can
A2 CAMBRIDGE GEOGRAPHY: GLOBAL INTERDEPENDENCE - TRADE FLOWS AND TRADING PATT...George Dumitrache
Global trade is worth trillions annually and involves the import and export of goods and services across international borders. Comparative advantage, as developed by David Ricardo, states that countries benefit by specializing in and trading goods and services they can produce relatively more cheaply. However, developing countries often face disadvantages like dependence on primary commodities and unfavorable terms of trade, though regional trade agreements and foreign investment can help increase trade and development.
A2 Human Geography - Economic transitionnazeema khan
This document provides information about economic transitions and changes in employment structures in different countries and regions. It discusses:
- The primary, secondary, tertiary, and quaternary sectors and how employment has shifted away from primary and secondary towards tertiary and quaternary.
- How employment structures have changed in high-income countries (HICs) due to outsourcing and a shift to services, resulting in HICs being called post-industrial societies.
- Differences in employment structures between low-income countries (LICs), newly industrialized countries (NICs), and HICs, and how structures have changed over time.
1) The document discusses atmospheric circulation and how differences in air pressure create wind patterns around the world.
2) It describes the trade winds that were discovered by Columbus and helped early explorers sail to destinations in the Americas and around the Cape of Good Hope in Africa.
3) The tricellular model proposed by Ferrel explains the global circulation pattern involving the Hadley cell, Ferrel cell, and polar cell that drive the trade winds and westerlies.
The Soufrière Hills volcano on the island of Montserrat erupted in 1995 due to its location on a destructive plate boundary, where the Atlantic oceanic plate is subducting under the Caribbean continental plate. As magma rose from the subducting plate it formed the composite Soufrière Hills volcano. In June 1997, the volcano's dome collapsed, sending pyroclastic flows down the mountain that engulfed villages, killing 19 people. The eruption destroyed homes and infrastructure across the southern half of the island.
CAMBRIDGE GEOGRAPHY AS EXTRA REVISION - EXAM STYLE QUESTIONS 2 - ATMOSPHERE A...George Dumitrache
Insolation refers to the solar radiation received from the sun, and albedo is the proportion of solar radiation reflected by a surface. Insolation would be greater and albedo lower in a tropical rainforest compared to a polar ice cap due to differences in surface reflectivity. Coastal areas may have higher temperatures than continental areas at the same latitude due to the moderating influence of bodies of water on temperature. Aspect, or the direction a slope faces, can also impact temperature, with sunnier south-facing slopes being warmer than north-facing slopes. The passage also defines dry adiabatic lapse rate and saturated adiabatic lapse rate, and explains how an understanding of lapse rates can
A2 CAMBRIDGE GEOGRAPHY: GLOBAL INTERDEPENDENCE - TRADE FLOWS AND TRADING PATT...George Dumitrache
Global trade is worth trillions annually and involves the import and export of goods and services across international borders. Comparative advantage, as developed by David Ricardo, states that countries benefit by specializing in and trading goods and services they can produce relatively more cheaply. However, developing countries often face disadvantages like dependence on primary commodities and unfavorable terms of trade, though regional trade agreements and foreign investment can help increase trade and development.
A2 Human Geography - Economic transitionnazeema khan
This document provides information about economic transitions and changes in employment structures in different countries and regions. It discusses:
- The primary, secondary, tertiary, and quaternary sectors and how employment has shifted away from primary and secondary towards tertiary and quaternary.
- How employment structures have changed in high-income countries (HICs) due to outsourcing and a shift to services, resulting in HICs being called post-industrial societies.
- Differences in employment structures between low-income countries (LICs), newly industrialized countries (NICs), and HICs, and how structures have changed over time.
1) The document discusses atmospheric circulation and how differences in air pressure create wind patterns around the world.
2) It describes the trade winds that were discovered by Columbus and helped early explorers sail to destinations in the Americas and around the Cape of Good Hope in Africa.
3) The tricellular model proposed by Ferrel explains the global circulation pattern involving the Hadley cell, Ferrel cell, and polar cell that drive the trade winds and westerlies.
Rocks form through three main processes: igneous, sedimentary, and metamorphic. Igneous rocks form when magma or lava cools and crystallizes. Sedimentary rocks form through the compaction and cementation of sediments over time. Metamorphic rocks were originally igneous or sedimentary rocks that were subjected to heat and pressure within the Earth, transforming their composition and structure.
13.1 Global Interdependence: Trade flows and trading patternsGeorge Dumitrache
Trade involves the exchange of goods and services between countries. Imports are purchased from other nations while exports are sold abroad. A country's balance of trade depends on whether it imports or exports more. Global trade patterns are influenced by factors like resource distribution, location, and trade agreements. While trade allows nations to specialize, many developing countries face unequal terms of trade and dependency on specific goods or partners. International organizations aim to promote free and fair trade globally.
AS GEOGRAPHY - ROCKS AND WEATHERING: WEATHERING AND ROCKSGeorge Dumitrache
Physical weathering breaks rocks into smaller pieces through processes like heating and cooling or wetting and drying. Chemical weathering alters the mineral composition of rocks through reactions with water and acids. Limestone landscapes feature karst topography with features like caves, sinkholes, and limestone pavements formed by the dissolution of calcium carbonate in the rocks. Granite weathers through freeze-thaw action and hydrolysis, forming tors and soil. The rate and type of weathering depends on climate, rock type, relief, vegetation and other factors.
The document discusses different tropical environments and climates. It begins by explaining that the Inter Tropical Convergence Zone (ITCZ) on average is located about 50 north of the equator but varies seasonally based on the sun's position. It then states that the ITCZ is the most important factor in the migration of low pressure belts and seasonal shifts in tropical rains. It goes on to briefly describe the climates of tropical rainforests, tropical monsoons, and tropical savannas.
A2 CAMBRIDGE GEOGRAPHY: CHARACTERISTICS AND FORMATION OF COASTAL LANDFORMSGeorge Dumitrache
A2 CAMBRIDGE GEOGRAPHY: CHARACTERISTICS AND FORMATION OF COASTAL LANDFORMS. It contains: the formation of erosional landforms: cliffs and wave-cut platforms, caves, arches and stacks
Learners should be able to explain the formation of depositional landforms: beaches in cross section (profile) and plan, swash and drift aligned beaches, simple and compound spits, tombolos, offshore bars, barrier beaches, coastal dunes, tidal sedimentation in estuaries, coastal saltmarshes and mangroves, the role of sea level change in the formation of coastal landforms.
1. An earthquake occurs when built-up tension along fault lines in the Earth's crust is suddenly released, causing the ground to shake.
2. The effects of an earthquake depend on several factors, including its magnitude on the Richter scale, distance from the epicenter, and the level of development in the affected area.
3. The 1995 Kobe earthquake in Japan caused over 30,000 injuries, left over 300,000 homeless as buildings collapsed, and led to long-term economic and social impacts as the city was rebuilt.
This document discusses erosional and depositional landforms caused by sea waves. It describes how sea waves erode coastal rocks through cracks and breaking pieces, forming sea cliffs, caves, arches and stacks. Sea caves are formed by wave erosion carving holes in the coastline. Arches are formed when sea caves on either side join together. Stacks remain when arch roofs collapse. Deposition by waves temporarily deposits sand and soil to form beaches. In conclusion, sea waves cause significant morphological changes along the shoreline through both erosional and depositional processes.
This document summarizes earth flows, which are a type of slow-moving landslide. Earth flows involve soil and weathered rock moving downhill like a fluid. They can range from a few square meters to several hectares in size. Earth flows often begin as slumps and do not move very quickly. Areas with clay, fine sand, silt or pyroclastic materials are susceptible to earth flows when the ground becomes saturated with water. Heavy rains, volcanic eruptions and earthquakes can all trigger earth flows. Methods to reduce earth flows include afforestation, reforestation, terracing slopes, covering landslides with impermeable membranes, and draining surface and ground water away from susceptible areas.
The document provides guidance on preparing for and taking the Unit 2 Geographical Investigations exam. It outlines that students will need to study two topics from a choice of four, and the exam will consist of answering two questions, one for each topic studied. It emphasizes the importance of fieldwork, research, and applying these skills to exam questions. It also provides tips for achieving high marks, such as focusing answers on the questions, using resources effectively, and incorporating fieldwork experiences.
A2 Geography Revision for Coastal Environments, subchapter 8.1 Waves Marine and Subaerial Processes. It is suitable for Year 13 Geography, Cambridge Examination in November 2016. It contains: key terms and definitions, a topic summary, sketches and descriptions, additional work (6 questions for testing your knowledge) and some suggested websites.
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - SUSTAINABLE MANAGEMENT IN HAZARDOUS ENVIRONMENTS. It contain the case study about Bioengineering in Malaysia.
This document provides an introduction to climatology, including definitions of key terms and branches of the field. It discusses how climatology studies the atmosphere and spatial patterns of climate. Climatology is related to both meteorology, which deals with day-to-day weather, and geography, which studies spatial climate distributions. The document also outlines the major layers of the atmosphere and characteristics of atmospheric gases like carbon dioxide and ozone.
This document discusses weather patterns associated with fronts and cyclones. It describes how weather changes as cold fronts and warm fronts approach and pass through a region. Cold fronts bring rapid weather changes like thunderstorms, while warm fronts pass more slowly with steady precipitation. Occluded and stationary fronts are associated with large areas of rainy weather. The document also outlines the four stages of cyclogenesis as a low pressure system develops - early, open, occluded, and dissolving stages - and the weather patterns at each stage.
The document discusses the four sectors of the economy: primary, secondary, tertiary, and quaternary. The primary sector involves agriculture and extraction of natural resources. The secondary sector processes raw materials into manufactured goods. The tertiary sector provides services. The quaternary sector offers information services. Employment structures have changed over time and differ between countries, with developed nations having more employment in the service sectors than agriculture and industry. Factors like resources, infrastructure, labor, and incentives influence where industries locate.
The document discusses 10 key concepts in geomorphology. It begins by defining geomorphology as the study of landforms and their formation and development. It then explains each concept in 1-2 paragraphs with examples. The concepts are: 1) Uniformitarianism, 2) Role of geologic structure, 3) Differential erosion rates, 4) Distinct landforms from geomorphic processes, 5) Geomorphic cycles, 6) Complex geomorphic evolution, 7) Young topography, 8) Impact of Pleistocene climate change, 9) Role of climate on processes, 10) Historical approach. The document concludes with a quick review of the 10 concepts.
Earthquakes are caused by both natural and human factors. Naturally, they result from the slow buildup of pressure along tectonic plate boundaries. Human causes include coal mining, construction of tall buildings, and dams. There are four main types of earthquakes classified by their origin. Earthquakes produce different types of seismic waves that cause damage. Mitigation efforts aim to reduce risks through regulations, education, and preparedness. At personal and government levels, precautions include earthquake-proof building techniques, emergency plans, and response coordination. Scientists study various prediction methods but cannot reliably forecast specific quakes. Developing countries often experience greater losses due to infrastructure and resources. Historic quakes in Haiti, San Francisco, and Chile caused
Slides on Weathering and Erosion for Irish Junior Cert students. Deals with various types of weathering and Karst landscapes, using the Burren as an example.
Weathering and erosion break down Earth's crust into smaller pieces through physical and chemical processes. Physical weathering breaks rocks into smaller pieces through external forces like frost wedging, friction, and animal burrowing. Chemical weathering uses chemical processes like water dissolving rock, oxygen combining with iron to form rust, and carbon dioxide forming carbonic acid to break down rock materials. Biological weathering also contributes through actions of plant roots and animal burrowing.
Rocks form through three main processes: igneous, sedimentary, and metamorphic. Igneous rocks form when magma or lava cools and crystallizes. Sedimentary rocks form through the compaction and cementation of sediments over time. Metamorphic rocks were originally igneous or sedimentary rocks that were subjected to heat and pressure within the Earth, transforming their composition and structure.
13.1 Global Interdependence: Trade flows and trading patternsGeorge Dumitrache
Trade involves the exchange of goods and services between countries. Imports are purchased from other nations while exports are sold abroad. A country's balance of trade depends on whether it imports or exports more. Global trade patterns are influenced by factors like resource distribution, location, and trade agreements. While trade allows nations to specialize, many developing countries face unequal terms of trade and dependency on specific goods or partners. International organizations aim to promote free and fair trade globally.
AS GEOGRAPHY - ROCKS AND WEATHERING: WEATHERING AND ROCKSGeorge Dumitrache
Physical weathering breaks rocks into smaller pieces through processes like heating and cooling or wetting and drying. Chemical weathering alters the mineral composition of rocks through reactions with water and acids. Limestone landscapes feature karst topography with features like caves, sinkholes, and limestone pavements formed by the dissolution of calcium carbonate in the rocks. Granite weathers through freeze-thaw action and hydrolysis, forming tors and soil. The rate and type of weathering depends on climate, rock type, relief, vegetation and other factors.
The document discusses different tropical environments and climates. It begins by explaining that the Inter Tropical Convergence Zone (ITCZ) on average is located about 50 north of the equator but varies seasonally based on the sun's position. It then states that the ITCZ is the most important factor in the migration of low pressure belts and seasonal shifts in tropical rains. It goes on to briefly describe the climates of tropical rainforests, tropical monsoons, and tropical savannas.
A2 CAMBRIDGE GEOGRAPHY: CHARACTERISTICS AND FORMATION OF COASTAL LANDFORMSGeorge Dumitrache
A2 CAMBRIDGE GEOGRAPHY: CHARACTERISTICS AND FORMATION OF COASTAL LANDFORMS. It contains: the formation of erosional landforms: cliffs and wave-cut platforms, caves, arches and stacks
Learners should be able to explain the formation of depositional landforms: beaches in cross section (profile) and plan, swash and drift aligned beaches, simple and compound spits, tombolos, offshore bars, barrier beaches, coastal dunes, tidal sedimentation in estuaries, coastal saltmarshes and mangroves, the role of sea level change in the formation of coastal landforms.
1. An earthquake occurs when built-up tension along fault lines in the Earth's crust is suddenly released, causing the ground to shake.
2. The effects of an earthquake depend on several factors, including its magnitude on the Richter scale, distance from the epicenter, and the level of development in the affected area.
3. The 1995 Kobe earthquake in Japan caused over 30,000 injuries, left over 300,000 homeless as buildings collapsed, and led to long-term economic and social impacts as the city was rebuilt.
This document discusses erosional and depositional landforms caused by sea waves. It describes how sea waves erode coastal rocks through cracks and breaking pieces, forming sea cliffs, caves, arches and stacks. Sea caves are formed by wave erosion carving holes in the coastline. Arches are formed when sea caves on either side join together. Stacks remain when arch roofs collapse. Deposition by waves temporarily deposits sand and soil to form beaches. In conclusion, sea waves cause significant morphological changes along the shoreline through both erosional and depositional processes.
This document summarizes earth flows, which are a type of slow-moving landslide. Earth flows involve soil and weathered rock moving downhill like a fluid. They can range from a few square meters to several hectares in size. Earth flows often begin as slumps and do not move very quickly. Areas with clay, fine sand, silt or pyroclastic materials are susceptible to earth flows when the ground becomes saturated with water. Heavy rains, volcanic eruptions and earthquakes can all trigger earth flows. Methods to reduce earth flows include afforestation, reforestation, terracing slopes, covering landslides with impermeable membranes, and draining surface and ground water away from susceptible areas.
The document provides guidance on preparing for and taking the Unit 2 Geographical Investigations exam. It outlines that students will need to study two topics from a choice of four, and the exam will consist of answering two questions, one for each topic studied. It emphasizes the importance of fieldwork, research, and applying these skills to exam questions. It also provides tips for achieving high marks, such as focusing answers on the questions, using resources effectively, and incorporating fieldwork experiences.
A2 Geography Revision for Coastal Environments, subchapter 8.1 Waves Marine and Subaerial Processes. It is suitable for Year 13 Geography, Cambridge Examination in November 2016. It contains: key terms and definitions, a topic summary, sketches and descriptions, additional work (6 questions for testing your knowledge) and some suggested websites.
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - SUSTAINABLE MANAGEMENT IN HAZARDOUS ENVIRONMENTS. It contain the case study about Bioengineering in Malaysia.
This document provides an introduction to climatology, including definitions of key terms and branches of the field. It discusses how climatology studies the atmosphere and spatial patterns of climate. Climatology is related to both meteorology, which deals with day-to-day weather, and geography, which studies spatial climate distributions. The document also outlines the major layers of the atmosphere and characteristics of atmospheric gases like carbon dioxide and ozone.
This document discusses weather patterns associated with fronts and cyclones. It describes how weather changes as cold fronts and warm fronts approach and pass through a region. Cold fronts bring rapid weather changes like thunderstorms, while warm fronts pass more slowly with steady precipitation. Occluded and stationary fronts are associated with large areas of rainy weather. The document also outlines the four stages of cyclogenesis as a low pressure system develops - early, open, occluded, and dissolving stages - and the weather patterns at each stage.
The document discusses the four sectors of the economy: primary, secondary, tertiary, and quaternary. The primary sector involves agriculture and extraction of natural resources. The secondary sector processes raw materials into manufactured goods. The tertiary sector provides services. The quaternary sector offers information services. Employment structures have changed over time and differ between countries, with developed nations having more employment in the service sectors than agriculture and industry. Factors like resources, infrastructure, labor, and incentives influence where industries locate.
The document discusses 10 key concepts in geomorphology. It begins by defining geomorphology as the study of landforms and their formation and development. It then explains each concept in 1-2 paragraphs with examples. The concepts are: 1) Uniformitarianism, 2) Role of geologic structure, 3) Differential erosion rates, 4) Distinct landforms from geomorphic processes, 5) Geomorphic cycles, 6) Complex geomorphic evolution, 7) Young topography, 8) Impact of Pleistocene climate change, 9) Role of climate on processes, 10) Historical approach. The document concludes with a quick review of the 10 concepts.
Earthquakes are caused by both natural and human factors. Naturally, they result from the slow buildup of pressure along tectonic plate boundaries. Human causes include coal mining, construction of tall buildings, and dams. There are four main types of earthquakes classified by their origin. Earthquakes produce different types of seismic waves that cause damage. Mitigation efforts aim to reduce risks through regulations, education, and preparedness. At personal and government levels, precautions include earthquake-proof building techniques, emergency plans, and response coordination. Scientists study various prediction methods but cannot reliably forecast specific quakes. Developing countries often experience greater losses due to infrastructure and resources. Historic quakes in Haiti, San Francisco, and Chile caused
Slides on Weathering and Erosion for Irish Junior Cert students. Deals with various types of weathering and Karst landscapes, using the Burren as an example.
Weathering and erosion break down Earth's crust into smaller pieces through physical and chemical processes. Physical weathering breaks rocks into smaller pieces through external forces like frost wedging, friction, and animal burrowing. Chemical weathering uses chemical processes like water dissolving rock, oxygen combining with iron to form rust, and carbon dioxide forming carbonic acid to break down rock materials. Biological weathering also contributes through actions of plant roots and animal burrowing.
Weathering breaks down rocks and minerals near Earth's surface through mechanical and chemical processes. Mechanical weathering physically breaks rocks into smaller pieces through frost wedging, thermal expansion and contraction, exfoliation, and abrasion by wind, water, or plant growth. Chemical weathering alters the chemical composition of rocks through dissolving, oxidation, and hydrolysis. Erosion transports weathered materials from their source through agents like water, wind, ice, and gravity, depositing sediments that form new rock layers over time.
Freeze-thaw weathering occurs when water enters cracks in rock and freezes, expanding by 9% and exerting pressure on the rock. When the ice melts and contracts, it causes further cracking. Over time, this process weakens the rock until it breaks apart into scree. Solution weathering dissolves limestone through slightly acidic water flowing through joints and pores in the rock, leaving formations like pavements, grykes, clints, and caverns. Areas like Dartmoor and Malham demonstrate these types of weathering on granite and limestone respectively.
Sedimentary rocks form through the weathering of pre-existing igneous, metamorphic and sedimentary rocks into sediments, which are then transported and deposited in layers. Weathering occurs through mechanical and chemical processes, with the rate controlled by factors like climate, rock type, and topography. Erosion removes the weathered sediments, which are transported by agents such as water, wind, and ice before being deposited in environments like rivers, lakes, and oceans, where they may eventually lithify to form sedimentary rock.
This document discusses several key concepts in plate tectonics:
- Faults are fractures in the Earth's crust where measurable movement has occurred. Trenches form from fault movements between converging plates.
- Plates are composed of continental and oceanic crust. Plate tectonics refers to the movement of these crustal plates.
- Alfred Wegener first proposed the continental drift theory that the world's continents were once joined together in a supercontinent called Pangaea.
Weathering refers to the breakdown of rocks into smaller pieces through mechanical, chemical, or biological processes without transportation, while erosion includes the transportation of weathered rock material by agents such as wind, water, or ice. This document describes three types of weathering - mechanical, chemical, and biological - and provides examples of specific weathering processes, including freeze-thaw action, salt crystallization, carbonation, hydration, oxidation, and hydrolysis. Images show examples of weathering patterns from these processes in various rock formations around Ireland.
Mechanical, chemical, and biological processes all contribute to weathering of rocks. Mechanical weathering breaks rocks down physically through freezing and thawing of water or expansion and contraction from temperature changes. Chemical weathering uses chemical reactions like oxidation and hydrolysis that break bonds between minerals, especially when aided by water. Biological weathering is caused by living organisms like plant roots that grow into cracks and widen them over time.
Limestone is a sedimentary rock composed largely of calcium carbonate. It forms from skeletal fragments of marine organisms and makes up about 10% of all sedimentary rocks. Limestone erodes over thousands to millions of years through water and weak acids, forming caves and karst landscapes. It has many uses including building material, road base, fillers, and feedstock for other materials. Stalactites form on cave ceilings through dripping water depositing calcium carbonate over time.
This document defines and describes the main types of weathering processes that occur at the Earth's surface: mechanical, chemical, and biological. Mechanical weathering involves physical breakdown through processes like frost wedging and abrasion without changing the rock's chemical composition. Chemical weathering decomposes rocks through reactions with substances like carbon dioxide, water, and oxygen. Biological weathering disintegrates rocks through organism activities like plant roots, lichen/algae growth, and burrowing. Different rock types and climates result in variable weathering rates.
This document contains summary notes on chemistry topics for a GCSE science course. It covers the fundamental ideas in chemistry including atoms, the periodic table, and chemical reactions. It also discusses specific topics like limestone and building materials, metals and their uses, crude oil and fuels, and plant oils. For each topic, it provides an overview and defines key terms and concepts.
This document discusses chemical reactions presented in a chemistry class. It includes questions and answers about experiments demonstrating different chemical reactions between substances like iron and copper sulfate, magnesium and oxygen, hydrogen peroxide and manganese dioxide, vinegar and baking soda, and copper sulfate and sodium hydroxide. The reactions produce substances like iron sulfate, copper, magnesium oxide, water, oxygen gas, sodium acetate, carbon dioxide, copper hydroxide, and sodium sulfate. The document also defines reactants and products, and shows how to write chemical equations using symbolic representations of the substances in the reactions.
11 Chap 6 Chemical Weathering (Rashmi Shammi).pptxRanasingh41
Rashmi Sammi presented on the topic of chemical weathering. The objectives were to understand the concept of chemical weathering, learn about its different types, and understand the process. Teaching methods included question and answer, lecture, audiovisual aids using ICT tools, and demonstrations. Chemical weathering changes rock composition through chemical reactions when water interacts with minerals. The major types of chemical weathering are solution, hydration, oxidation, and carbonation which are influenced by factors like temperature, surface area, and water availability. Students were given an assignment to define chemical weathering and explain its different types.
This document provides information about a science project submitted by Aditya Sha of class 10th. It discusses various topics related to chemical reactions including word equations, balanced chemical equations, types of chemical reactions, and signs of chemical reactions. It also covers corrosion, rancidity, and their causes and effects. The document recognizes several teachers and parents who provided support for the project.
Classic, mini chemistry experiments- some require materials typically found in a high school chemistry lab, while others are extremely simple. Very straightforward!
Effluent Treatment Plant in Oil Refineries.pptxHritwikGhosh
The document describes the processes involved in an effluent treatment plant (ETP). An ETP treats industrial wastewater through primary, secondary, and tertiary treatments to remove solids, chemicals, and organic substances before reuse or safe disposal. The major treatment stages include physio-chemical processes like oil separation, biological treatment using activated sludge and biotowers, and tertiary treatments like hardness removal. Sludge generated is thickened for volume reduction through sedimentation tanks and centrifuges. The overall ETP process aims to safely treat industrial wastewater for environmental and public health purposes.
The document provides an overview of the unit on microbiology, covering topics such as bioremediation, acid mine drainage, enhanced metal recovery through bioleaching, wastewater microbiology, solid waste microbiology related to landfills, and anaerobic degradation phases. It then discusses in more detail acid mine drainage chemistry, impacts, bioleaching processes, the four phases of anaerobic digestion, and mechanisms of antimicrobial resistance.
Corrosion is the gradual destruction of a metal due to reactions with its environment. Over time, corrosion changes the appearance of the metal as it breaks down and becomes weaker. Coating metals with paint or chemicals protects them from corrosion, but damage to these coatings allows corrosion to occur. Rusting refers specifically to the corrosion of iron through a reaction of iron with oxygen and water to form hydrated iron oxide. Factors like salt can increase the rate of corrosion. Methods of preventing corrosion include covering metals with grease, attaching zinc, painting, or coating with tin.
The document discusses different types of chemical reactions including acid-base reactions where an acid and base react to form a salt and water, precipitation reactions where insoluble compounds form solid precipitates, and oxidation-reduction reactions where electrons are lost or gained. Examples of each type of reaction are provided and rules for determining oxidation states and predicting products are explained.
The document describes the copper cycle, which involves a series of chemical reactions that transform copper between different forms. Specifically, copper is exposed to various chemicals to change it into copper nitrate, hydroxide, oxide, and sulfate, before being transformed back into its original elemental form. The alternating reactions demonstrate copper's ability to cycle between ionic and elemental states in biological and environmental systems.
This document discusses various issues related to water pollution. It begins by describing different industrial uses of water, such as for cooling, processing, and transport. It then discusses how industrial activities and mining can pollute surface and groundwater through runoff, spills, and aerial pollution. Next, it examines how pollution can disrupt aquatic ecosystems by overloading their self-cleaning capacity. It proceeds to define various water pollutants and parameters used to measure water quality, such as dissolved oxygen, organic content, nutrients, and heavy metals. Finally, it analyzes specific pollution problems including deoxygenation, acid mine drainage, eutrophication, and heavy metal contamination from sources like road runoff.
This features the types of chemical reactions: Combustion, Neutralization, Precipitation and RedOx Reactions.
There are sample in each of the type of reaction that can help the learners understand more about each type.
Microorganisms have the ability to utilize hydrocarbons (HCs) as an energy source and can play a role in biodegrading petroleum pollution. The document discusses several factors that influence the biodegradation of petroleum HCs by microbes, including the physical state of the oil, temperature, nutrients, oxygen, salinity, and pressure. Mix populations of diverse bacteria and fungi that can degrade different components of petroleum HCs are generally more efficient at the biodegradation process.
ECOTOXICAL ASSESSMENT OF BIODEGRADATION Meet Zadafiya
This document discusses ecotoxicological assessment of biodegradable polymers. It contains sections on end of life scenarios of biodegradable polymers including aerobic and anaerobic conditions. It also discusses biodegradation during organic recycling through industrial composting, home composting, and anaerobic digestion. Another section covers investigating polymer biodegradation and identifying intermediates. The document ends with sections on ecotoxicological assessment of biodegradation intermediates in aquatic environments through impacts on bacteria, algae, crustaceans and fish, and in terrestrial environments through impacts on bacteria, invertebrates, plants and vertebrates.
Biosoption of heavy metals by orange peelAbbas Kazi
Biosorption uses biological materials like bacteria, fungi, and orange peel to remove heavy metals from wastewater. Orange peel is a good biosorbent because it contains cellulose and pigments with hydroxyl groups that can adsorb metals. This document outlines experiments examining orange peel's ability to remove copper, cadmium, lead, zinc, and nickel. The effects of pH, contact time, initial concentration, adsorbent dosage, and ionic strength on adsorption were studied. Adsorption increased with pH and adsorbent amount and reached equilibrium within 20 minutes. Adsorption also fit the Langmuir isotherm model well, indicating monolayer adsorption onto the
Everyday activities involve many redox reactions. Metals corrode through oxidation when exposed to oxygen and moisture. Bleach removes color through redox reactions that oxidize dyes. Breathalyzer tests use the oxidation of ethanol to change a solution from orange to green. Cut fruits brown through enzymatic oxidation reactions with oxygen in the air. Respiration, combustion, photosynthesis, and photography all involve important redox reactions as well.
Carbon is essential for life and is present in many biological molecules like proteins, nucleic acids, lipids, and carbohydrates. It cycles between the atmosphere, ocean, living things, and geological reservoirs as part of the global carbon cycle. The carbon cycle involves photosynthesis fixing carbon from the air or water into organic compounds, respiration and decomposition releasing it back, and geological processes like fossil fuel formation, limestone creation and erosion, and volcanic activity moving it between air, water, and rocks over long time periods.
The document discusses the carbonate system and chemical weathering. It describes the carbonate equilibrium reactions and species like carbonic acid, bicarbonate, and carbonate that are involved. Chemical weathering plays an important role in regulating atmospheric carbon dioxide and climate by slowly breaking down continental rocks and sequestering carbon over millions of years. Factors like temperature, precipitation, and vegetation influence chemical weathering rates and provide negative feedback that moderates global temperatures.
The document discusses acids and bases in several contexts. It covers acid rain and its environmental effects. It also discusses antacids and how they are used to treat excess stomach acid. Additionally, it examines the roles of acids and bases in industry, the home, health, and disease. It provides examples of commonly used acids like sulfuric acid and bases like lime. Finally, it includes a quiz to test the reader's understanding.
This document provides information about study resources for exams, including quick study options with over 400 YouTube videos and 200 slideshare presentations covering 11 subjects, as well as comprehensive studying with 250 lessons per subject broken into modules and over 30,000 test items. Users can create an account to access these resources through a Moodle online learning platform by searching courses or topics.
This document outlines the key concepts and examples for matrices including: addition and subtraction of matrices with the same dimensions; scalar multiplication by multiplying each element of the matrix by the scalar; matrix multiplication where the number of columns of the first matrix equals the number of rows of the second matrix; determinants of 2x2 matrices; inverse matrices for non-singular 2x2 matrices; solving systems of equations using matrices; and geometric transformations using matrices including rotation, reflection, translation and examples of applying transformations.
This document contains 6 presentations on vectors:
1) Identifying equivalent and opposite vectors in a diagram
2) Calculating components of vectors
3) Writing vector expressions in terms of other vectors
4) Illustrating vector addition and subtraction on a grid
5) Expressing vectors in terms of other vectors using properties of midpoints
6) Expressing vectors in terms of other vectors and proving collinearity using properties of parallelograms
Math unit36 contructions and enlargementseLearningJa
This document discusses geometric transformations including lines of symmetry, rotational symmetry, enlargements, and finding the scale factor and center of enlargement. Lines of symmetry and orders of rotational symmetry are identified for different shapes. Enlargements are performed using given scale factors and centers. The ratio of areas for different enlargements is calculated. Scale factors and centers of enlargement are determined for shapes.
This document covers trigonometric concepts and problems involving right-angled triangles, bearings, and trigonometric functions. It includes 7 presentations on finding angles in right triangles using trig functions, problems using trigonometry including elevation and depression, the sine rule, cosine rule, problems with bearings, and trig functions. Examples are provided for each topic to demonstrate how to set up and solve various trigonometric problems.
This document covers the topics of congruence, similarity, and ratios between similar shapes. It includes 4 tests for determining if triangles are congruent based on side lengths and angles. It also discusses identifying similar shapes and using corresponding parts of similar triangles to determine unknown lengths and angles. Finally, it examines how linear dimensions, areas, and volumes are scaled between similar cuboids based on common scale factors.
Math unit32 angles, circles and tangentseLearningJa
This document contains 8 presentations on the topics of angles, circles, and tangents. It includes definitions, results, and examples related to compass bearings, angles formed with circles, properties of circles and tangents, and the relationships between angles on circles and chords. Practice problems are provided for students to apply the concepts to geometric diagrams.
Math unit29 using graphs to solve equationseLearningJa
This document discusses using graphs to solve equations. It covers solving simultaneous equations by graphing the lines and finding their intersection point. It also discusses graphs of quadratic, cubic, and reciprocal functions, including their key characteristics and shapes. Examples of each type of function are shown. The document concludes by discussing using graphs to find specific values or intervals related to equations.
This document contains 6 presentations on functions, mappings, and domains:
1) It introduces functions, mappings, and domains.
2) It further explores functions, mappings, and domains with examples.
3) It provides another example and asks about domain and range.
4) It covers composite functions, finding functions of other functions.
5) It introduces the concept of inverse functions.
6) It gives another example of finding the inverse of a function.
This document covers straight lines and their properties including positive and negative gradient, the relationship between perpendicular lines, using graphs to determine speed and distance, and finding equations of lines. It provides examples of calculating gradient, determining if two lines are perpendicular, finding speed from a distance-time graph, and deriving equations of lines given points or being parallel/perpendicular to another line. The content builds understanding of key concepts involving straight lines through worked examples.
This document discusses solving inequalities and linear programming problems. It covers inequalities on a number line, solving linear inequalities, inequalities involving quadratic terms, using a graphical approach, and linear programming problems. Examples are provided for illustrating inequalities on number lines, solving various types of inequalities, finding the region defined by inequality constraints on a graph, and analyzing a linear programming problem about profit from cricket club uniform sales to determine the minimum possible profit.
This document contains 6 presentations on the topic of coordinates:
1. Positive coordinates and plotting points in a plane
2. Writing coordinates of points and identifying locations
3. Plotting straight lines by connecting points
4. Plotting curves by connecting points in a smooth curve
5. Finding the midpoint of a line segment by averaging the x and y coordinates
6. Three-dimensional coordinates by extending points into the z-axis
This document contains summaries of 8 presentations about formulas:
1. Using formulas to calculate the perimeter and area of a rectangle given the length and width.
2. Constructing a formula to calculate an engineer's charge based on a fixed fee plus an hourly rate multiplied by hours worked.
3. Reviewing rules for performing calculations with negative numbers.
4. Using information provided to calculate temperature differences between various cities.
5. Substituting values into a formula to calculate the length of a metal rod at different temperatures.
6. Substituting values into a more complex formula involving fractions to calculate a focal length.
7. Rewriting a formula connecting Celsius and Fahrenheit
This document outlines 8 presentations covering algebraic concepts taught in Unit 22. The presentations include simplifying expressions, solving simple and linear equations, equations in context, algebraic manipulation, and algebraic fractions. Each presentation provides example problems and solutions to illustrate the concepts and skills covered.
This document contains explanations and examples related to probability concepts. It includes 4 presentations: 1) Simple Probability, 2) Probabilities, 3) Determining Probabilities, and 4) Misconceptions. The presentations provide examples of calculating probabilities of events, common probability misconceptions, and explanations for why the misconceptions are incorrect.
The document contains information about measures of variation and distributions, including:
1) A table showing the age distribution of Nigeria's population in 1991, with the lower quartile around 11 years, median around 24 years, and upper quartile around 40.5 years.
2) A table with test marks for 70 students, including constructing a cumulative frequency curve and determining that 28 students passed with a mark over 47.
3) Box and whisker plots are constructed to represent the goals scored in football matches by two teams, comparing their median, quartiles, and range.
4) Standard deviation is defined as a measure of spread from the mean, and the standard deviations of three data sets S1, S2,
Math unit20 probability of one or more eventseLearningJa
This document is a presentation on probability of two or more events. It includes sections on probability outcomes for rolling a dice and flipping a coin simultaneously, rolling two dice and adding the scores, using tree diagrams to calculate probabilities of outcomes from rolling two dice or drawing balls from containers. It also addresses common misconceptions about probability, such as assuming the number of possible outcomes corresponds to the probability of a specific outcome, or that order matters in independent events. The presentation provides examples and prompts users to complete probability calculations to demonstrate their understanding of fundamental probability concepts involving two or more random events.
The document discusses different data presentation methods including pie charts, line graphs, histograms, and histograms with unequal class intervals. It provides examples of how to represent various data sets visually using these different graph types, including steps for constructing the graphs, calculating values, and interpreting the results.
This document contains 4 presentations on volume, sectors, and arcs. The first presentation defines the formulas for calculating the volumes of cubes, cuboids, cylinders, and triangular prisms. The second presentation covers the relationships between mass, volume, and density. The third presentation provides the formulas for finding the areas of sectors and arc lengths of circles. The final presentation defines the volume formulas for pyramids, cones, and spheres and includes an example problem calculating the height of a cone with the same volume and radius as a sphere.
A review of the growth of the Israel Genealogy Research Association Database Collection for the last 12 months. Our collection is now passed the 3 million mark and still growing. See which archives have contributed the most. See the different types of records we have, and which years have had records added. You can also see what we have for the future.
Strategies for Effective Upskilling is a presentation by Chinwendu Peace in a Your Skill Boost Masterclass organisation by the Excellence Foundation for South Sudan on 08th and 09th June 2024 from 1 PM to 3 PM on each day.
Reimagining Your Library Space: How to Increase the Vibes in Your Library No ...Diana Rendina
Librarians are leading the way in creating future-ready citizens – now we need to update our spaces to match. In this session, attendees will get inspiration for transforming their library spaces. You’ll learn how to survey students and patrons, create a focus group, and use design thinking to brainstorm ideas for your space. We’ll discuss budget friendly ways to change your space as well as how to find funding. No matter where you’re at, you’ll find ideas for reimagining your space in this session.
This slide is special for master students (MIBS & MIFB) in UUM. Also useful for readers who are interested in the topic of contemporary Islamic banking.
বাংলাদেশের অর্থনৈতিক সমীক্ষা ২০২৪ [Bangladesh Economic Review 2024 Bangla.pdf] কম্পিউটার , ট্যাব ও স্মার্ট ফোন ভার্সন সহ সম্পূর্ণ বাংলা ই-বুক বা pdf বই " সুচিপত্র ...বুকমার্ক মেনু 🔖 ও হাইপার লিংক মেনু 📝👆 যুক্ত ..
আমাদের সবার জন্য খুব খুব গুরুত্বপূর্ণ একটি বই ..বিসিএস, ব্যাংক, ইউনিভার্সিটি ভর্তি ও যে কোন প্রতিযোগিতা মূলক পরীক্ষার জন্য এর খুব ইম্পরট্যান্ট একটি বিষয় ...তাছাড়া বাংলাদেশের সাম্প্রতিক যে কোন ডাটা বা তথ্য এই বইতে পাবেন ...
তাই একজন নাগরিক হিসাবে এই তথ্য গুলো আপনার জানা প্রয়োজন ...।
বিসিএস ও ব্যাংক এর লিখিত পরীক্ষা ...+এছাড়া মাধ্যমিক ও উচ্চমাধ্যমিকের স্টুডেন্টদের জন্য অনেক কাজে আসবে ...
This presentation was provided by Steph Pollock of The American Psychological Association’s Journals Program, and Damita Snow, of The American Society of Civil Engineers (ASCE), for the initial session of NISO's 2024 Training Series "DEIA in the Scholarly Landscape." Session One: 'Setting Expectations: a DEIA Primer,' was held June 6, 2024.
How to Setup Warehouse & Location in Odoo 17 InventoryCeline George
In this slide, we'll explore how to set up warehouses and locations in Odoo 17 Inventory. This will help us manage our stock effectively, track inventory levels, and streamline warehouse operations.
Walmart Business+ and Spark Good for Nonprofits.pdfTechSoup
"Learn about all the ways Walmart supports nonprofit organizations.
You will hear from Liz Willett, the Head of Nonprofits, and hear about what Walmart is doing to help nonprofits, including Walmart Business and Spark Good. Walmart Business+ is a new offer for nonprofits that offers discounts and also streamlines nonprofits order and expense tracking, saving time and money.
The webinar may also give some examples on how nonprofits can best leverage Walmart Business+.
The event will cover the following::
Walmart Business + (https://business.walmart.com/plus) is a new shopping experience for nonprofits, schools, and local business customers that connects an exclusive online shopping experience to stores. Benefits include free delivery and shipping, a 'Spend Analytics” feature, special discounts, deals and tax-exempt shopping.
Special TechSoup offer for a free 180 days membership, and up to $150 in discounts on eligible orders.
Spark Good (walmart.com/sparkgood) is a charitable platform that enables nonprofits to receive donations directly from customers and associates.
Answers about how you can do more with Walmart!"
3. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
Students should be able to:
• define the terms chemical and biotic
weathering,
• explain the processes of chemical weathering
such as carbonation, oxidation and solution,
• discuss how different processes of chemical
weathering are influenced by factors such as
climate, rock type, and living organisms,
• understand the impact of chemical
weathering on rock surfaces.
3
4. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
ChemicalWeathering is the decay of rocks. It
occurs when rock minerals react with rain water,
moisture or air to alter the chemical composition
and structure of the rock.The original rock
minerals are changed to form new compounds
which leads to the decomposition of the rocks.
Types of chemical weathering are:
Oxidation
Solution
Carbonation
Biotic
4
5. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
WEATHERINGWEATHERING
Chemical WeatheringChemical Weathering
OxidationOxidation SolutionSolution CarbonationCarbonation BioticBiotic
5
6. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES ChemicalWeathering
What you need: lemon or lime juice, vinegar,
medicine droppers, two pieces each of
limestone, chalk, and quartzite.
What to do:
1. Put a few drops of lemon juice on one of each
of the three rock samples.
2. Put a few drops of vinegar on each of the other
three samples.
3. Look and listen carefully each time you add
the lemon juice or 1the vinegar.
6
7. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES Think about the questions and type your responses below.
You must be in Slide Show view to type and delete text.
7
Click for FeedbackClick for Feedback
8. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
What should have happened:
• Lemon juice and vinegar are both weak acids.
These mild acids can dissolve rocks that
contain calcium carbonate.
• The lemon juice and vinegar should have
bubbled or fizzed on the limestone and chalk,
which all contain calcium carbonate.
• There should not have been a reaction on the
quartz, which does not contain calcium
carbonate.
8
9. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES • Oxidation is the process in which oxygen
chemically combines with other substances.
• Oxidation occurs when rocks are exposed to
oxygen the air or water.The chemical addition
of oxygen to compounds in the rock can
weaken the structure of the rock.
• When iron compounds combine with oxygen
ferric oxide (iron oxide) is formed which gives
rocks a reddish brown tinge.
• Oxidation causes rocks to decay and crumble
easily.
• Oxidation is the process that causes metals to
rust .
9
10. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
10
Can you identify the areas where oxidation
has occurred?
In Slide Show view, type your
answer in the box below.
11. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
11
Describe what is taking place in the picture.
In Slide Show view,
type your answer in the
box below.
12. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES Rocks that dissolve easily in water are said to
be soluble.
Many minerals are soluble in water especially if
the water is acidic. Minerals such as rock salt
can be dissolved by water.
Most rain water and water in the soil are
slightly acid.When the minerals in rock
dissolve hollows are left within the rock
structure while the less soluble minerals
remain.
12
13. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES • Carbonation is a form of chemical weathering
which affects limestone. It operates like this:
• Carbonation takes place when carbon dioxide
in the atmosphere dissolves in rain water to
form carbonic acid.
• Rain water as a weak acid reacts with
limestone (calcium carbonate) and it becomes
soluble and dissolves in the water.
• The process of carbonation occurs along the
joins in the limestone and enlarge them.
13
14. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
A limestone pavement – notice the grooves and ridges
caused by solution of the limestone 14
15. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
15
Lichens are plants that
produce weak acids.
These plants often grow
on rocks. As they grow,
the acids they produce
seep into the rocks and
dissolve some of the
minerals resulting in
chemical weathering.
16. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES Are you ready to test yourself?
There are four multiple choice items that you
are required to do.
For each item, click on the letter of the correct
response and then click the button ‘NEXT
QUESTION’ to continue.
You must be in sldie show view to do the quiz.
Click the BEGIN QUIZ button to proceed.
16
BEGIN QUIZ!BEGIN QUIZ!
17. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES The general process by which rocks are broken down on
the Earth’s surface is called:
17
A. decompositionA. decomposition
B. erosionB. erosion
C. denudationC. denudation
D. weatheringD. weathering
FEEDBACKFEEDBACKFEEDBACKFEEDBACK
18. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
Question 1: The general process by which rocks
are broken down on the Earth’s surface is called:
Feedback
Weathering is the first stage in the break down of
rocks which are then picked up by agents of
erosion such as running water, the sea and
moving ice. All these processes result in
denudation.
18
NEXT QUESTIONNEXT QUESTIONNEXT QUESTIONNEXT QUESTION
19. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
The decomposition of rock from exposure to
water and atmospheric gases is known as:
19
A. Mechanical weatheringA. Mechanical weathering
D. Salt wedgingD. Salt wedging
C. DenudationC. Denudation
B. Chemical weatheringB. Chemical weathering
FEEDBACKFEEDBACKFEEDBACKFEEDBACK
20. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
Question 2: The decomposition of rock from
exposure to water and atmospheric gases is
known as:
Feedback
Chemical weathering results in the change in the
chemical composition of rocks this is brought
about by chemical reactions that occur in the
presence of oxygen and carbon dioxide.
20
NEXT QUESTIONNEXT QUESTIONNEXT QUESTIONNEXT QUESTION
21. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
Chemical weathering takes place most effectively
when it is:
21
A. Cold and dryA. Cold and dry
D. Dry all the timeD. Dry all the time
B. Cold and wetB. Cold and wet
C. Warm and wetC. Warm and wet
FEEDBACKFEEDBACKFEEDBACKFEEDBACK
22. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
Question 3: Chemical weathering takes place
most effectively when it is:
Feedback
Chemical weathering occurs because chemical
reactions are occurring on rock surfaces. Most
chemical reactions occur in the presence of
water and in warm temperatures.Thus warm
wet conditions are ideal settings for chemical
weathering.
22
NEXT QUESTIONNEXT QUESTIONNEXT QUESTIONNEXT QUESTION
23. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
Carbonic acid, the primary agent of chemical
weathering is produced by:
23
A. Plant rootsA. Plant roots
D. Oxygen reacting with iron compoundsD. Oxygen reacting with iron compounds
C. Bacteria that feeds on plant and animal remainsC. Bacteria that feeds on plant and animal remains
B. Carbon dioxide dissolving in rain waterB. Carbon dioxide dissolving in rain water
FEEDBACKFEEDBACKFEEDBACKFEEDBACK
24. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
Question 4: Carbonic acid, the primary agent of
chemical weathering is produced by:
Feedback
Rain water dissolves carbon dioxide from the air
as it passes through it rain water (H2O ) + carbon
dioxide (CO2) = mild carbonic acid (H2 CO3)
24
NEXT QUESTIONNEXT QUESTIONNEXT QUESTIONNEXT QUESTION
25. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES
The process in which oxygen chemically
combines with substances is:
25
B. DecompositionB. Decomposition
D. DenudationD. Denudation
C. CarbonationC. Carbonation
A. OxidationA. Oxidation
FEEDBACKFEEDBACKFEEDBACKFEEDBACK
26. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES Question 5: The process in which oxygen chemically
combines with substances is:
Feedback
Oxidation –is the chemical addition of oxygen to
compounds in rocks and it can weaken the structure of
rocks. Oxygen either dissolved in water or in the air
combines with minerals present in the rocks.
This type of weathering is also known as rusting as
the rock discolours to a reddish-brown colour.
26END OF QUIZEND OF QUIZEND OF QUIZEND OF QUIZ
27. WHAT IS CHEMICAL
WEATHERING?
WHAT IS CHEMICAL
WEATHERING?
1 - OXIDATION1 - OXIDATION
2 - SOLUTION2 - SOLUTION
3 - CARBONATION3 - CARBONATION
4 - BIOTIC4 - BIOTIC
QUIZQUIZ
OBJECTIVESOBJECTIVES You have reached the end of the quiz.
If you wish to review this lesson, go to the first
slide.
If you have finished viewing the lesson, click
the Close (X) button.
27
Editor's Notes
Read this before viewing as slide show.
Note. If you are using PowerPoint 2007, before you begin, look for the Security Warning below the ribbon, above this slide and click the Options button. In the Security Alert box, click “Enable This Content”
If you are using PowerPoint 2013, look below the ribbon. If you see a Security Warning, click Enable Content before viewing in Slide Show View.