The document discusses the water cycle and movement of water on and below Earth's surface. It describes key processes like infiltration, transpiration, precipitation, evaporation, and runoff. It also explains surface water features such as streams, valleys, floods, and drainage basins. Finally, it covers groundwater topics like aquifers, wells, springs, and karst topography.
Physical Geography Lecture 09 - Water Resources (Ground water and ice) 110716angelaorr
Movement and locations of water. Underground water. Soil water belt, subsurface flow. Percolation. Porosity and Permeability. Hydrologic Zones. Zone of aeration, zone of saturation, water table, effluent and influent condition. Zone of confined water, aquaclude, aquifer, artesian well. Waterless zone. Groundwater management. Groundwater management issues. Aquifer recharge, cone of depression, subsidence, groundwater contamination. The case of Venice Italy. Hydrothermal activity. Hot springs, geysers, fumaroles. Permafrost, melting permafrost. Glaciers, alpine and continental glaciers. Melting glaciers. Lakes. Destruction of the Aral Sea. Swamps and marshes. Streams.
Physical Geography Lecture 09 - Water Resources (Ground water and ice) 110716angelaorr
Movement and locations of water. Underground water. Soil water belt, subsurface flow. Percolation. Porosity and Permeability. Hydrologic Zones. Zone of aeration, zone of saturation, water table, effluent and influent condition. Zone of confined water, aquaclude, aquifer, artesian well. Waterless zone. Groundwater management. Groundwater management issues. Aquifer recharge, cone of depression, subsidence, groundwater contamination. The case of Venice Italy. Hydrothermal activity. Hot springs, geysers, fumaroles. Permafrost, melting permafrost. Glaciers, alpine and continental glaciers. Melting glaciers. Lakes. Destruction of the Aral Sea. Swamps and marshes. Streams.
Model Attribute Check Company Auto PropertyCeline George
In Odoo, the multi-company feature allows you to manage multiple companies within a single Odoo database instance. Each company can have its own configurations while still sharing common resources such as products, customers, and suppliers.
Ethnobotany and Ethnopharmacology:
Ethnobotany in herbal drug evaluation,
Impact of Ethnobotany in traditional medicine,
New development in herbals,
Bio-prospecting tools for drug discovery,
Role of Ethnopharmacology in drug evaluation,
Reverse Pharmacology.
We all have good and bad thoughts from time to time and situation to situation. We are bombarded daily with spiraling thoughts(both negative and positive) creating all-consuming feel , making us difficult to manage with associated suffering. Good thoughts are like our Mob Signal (Positive thought) amidst noise(negative thought) in the atmosphere. Negative thoughts like noise outweigh positive thoughts. These thoughts often create unwanted confusion, trouble, stress and frustration in our mind as well as chaos in our physical world. Negative thoughts are also known as “distorted thinking”.
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
How to Split Bills in the Odoo 17 POS ModuleCeline George
Bills have a main role in point of sale procedure. It will help to track sales, handling payments and giving receipts to customers. Bill splitting also has an important role in POS. For example, If some friends come together for dinner and if they want to divide the bill then it is possible by POS bill splitting. This slide will show how to split bills in odoo 17 POS.
This is a presentation by Dada Robert in a Your Skill Boost masterclass organised by the Excellence Foundation for South Sudan (EFSS) on Saturday, the 25th and Sunday, the 26th of May 2024.
He discussed the concept of quality improvement, emphasizing its applicability to various aspects of life, including personal, project, and program improvements. He defined quality as doing the right thing at the right time in the right way to achieve the best possible results and discussed the concept of the "gap" between what we know and what we do, and how this gap represents the areas we need to improve. He explained the scientific approach to quality improvement, which involves systematic performance analysis, testing and learning, and implementing change ideas. He also highlighted the importance of client focus and a team approach to quality improvement.
Palestine last event orientationfvgnh .pptxRaedMohamed3
An EFL lesson about the current events in Palestine. It is intended to be for intermediate students who wish to increase their listening skills through a short lesson in power point.
Synthetic Fiber Construction in lab .pptxPavel ( NSTU)
Synthetic fiber production is a fascinating and complex field that blends chemistry, engineering, and environmental science. By understanding these aspects, students can gain a comprehensive view of synthetic fiber production, its impact on society and the environment, and the potential for future innovations. Synthetic fibers play a crucial role in modern society, impacting various aspects of daily life, industry, and the environment. ynthetic fibers are integral to modern life, offering a range of benefits from cost-effectiveness and versatility to innovative applications and performance characteristics. While they pose environmental challenges, ongoing research and development aim to create more sustainable and eco-friendly alternatives. Understanding the importance of synthetic fibers helps in appreciating their role in the economy, industry, and daily life, while also emphasizing the need for sustainable practices and innovation.
The Indian economy is classified into different sectors to simplify the analysis and understanding of economic activities. For Class 10, it's essential to grasp the sectors of the Indian economy, understand their characteristics, and recognize their importance. This guide will provide detailed notes on the Sectors of the Indian Economy Class 10, using specific long-tail keywords to enhance comprehension.
For more information, visit-www.vavaclasses.com
How to Make a Field invisible in Odoo 17Celine George
It is possible to hide or invisible some fields in odoo. Commonly using “invisible” attribute in the field definition to invisible the fields. This slide will show how to make a field invisible in odoo 17.
3. 6.1 Running Water Water constantly moves among the oceans, the atmosphere, the solid Earth, and the biosphere. This unending circulation of Earth’s water supply is the water cycle. The Water Cycle
4. 6.1 Running Water Processes involved in the cycle are • infiltration —the movement of surface water into rock or soil through cracks and pore spaces • transpiration —the release of water into the atmosphere from plants through the ground • precipitation • evaporation • runoff The Water Cycle
5. 6.1 Running Water Balance in the water cycle means the average annual precipitation over Earth equals the amount of water that evaporates. Earth’s Water Balance
8. 6.1 Running Water The ability of a stream to erode and transport materials depends largely on its velocity. • Gradient is the slope or steepness of a stream channel. Streamflow
9. 6.1 Running Water • Channel Characteristics • Discharge of a stream is the volume of water flowing past a certain point in a given unit of time. - The stream channel is the course the water in a stream follows. - Shape, size, and roughness Streamflow
10. 6.1 Running Water • Cross-sectional view of a stream • From head (source) to mouth While gradient decreases between a stream’s headwaters and mouth, discharge increases. Profile - Profile is a smooth curve - Gradient decreases from the head to the mouth Changes from Upstream to Downstream
11. Profile • Factors that increase downstream - velocity - discharge • A tributary is a stream that empties into another stream. - channel size Changes from Upstream to Downstream 6.1 Running Water
13. Profile • Factors that decrease downstream include - gradient, or slope - channel roughness Changes from Upstream to Downstream 6.1 Running Water
15. • A stream in a broad, flat-bottomed valley that is near its base level often develops a course with many bends called meanders. Base Level • Lowest point to which a stream can erode • Two general types - ultimate — sea level - temporary, or local Changes from Upstream to Downstream 6.1 Running Water
16. Streams generally erode their channels, lifting loose particles by abrasion, grinding, and by dissolving soluble material. Erosion 6.2 The Work of Streams
17. Deposition occurs as streamflow drops below the critical settling velocity of a certain particle size. The deposits are called alluvium. Deltas are an accumulation of sediment formed where a stream enters a lake or ocean. A natural levee parallels a stream and helps to contain its waters, except during floodstage. A stream’s bedload is solid material too large to carry in suspension. The capacity of a stream is the maximum load it can carry. Deposition 6.2 The Work of Streams
18. Narrow Valleys • A narrow V-shaped valley shows that the stream’s primary work has been downcutting toward base level. • Features often include - rapids - waterfalls Stream Valleys 6.2 The Work of Streams
20. Wide Valleys • Stream is near base level. - Downward erosion is less dominant. - Stream energy is directed from side to side. • The floodplain is the flat, low-lying portion of a stream valley subject to periodic flooding. Stream Valleys 6.2 The Work of Streams
21. Wide Valleys • Features often include - meanders - cutoffs - oxbow lakes Stream Valleys 6.2 The Work of Streams
23. A flood occurs when the discharge of a stream becomes so great that it exceeds the capacity of its channel and overflows its banks. Measures to control flooding include artificial levees, flood control dams, and placing limits on floodplain development. Floods and Flood Control 6.2 The Work of Streams
25. A drainage basin is the land area that contributes water to a stream. A divide is an imaginary line that separates the drainage basins of one stream from another. Drainage Basins 6.2 The Work of Streams
26. Much of the water in soil seeps downward until it reaches the zone of saturation. The zone of saturation is the area where water fills all of the open spaces in sediment and rock. • Groundwater is the water within this zone. • The water table is the upper level of the saturation zone of groundwater. Distribution and Movement of Water Underground 6.3 Water Beneath the Surface
27. Movement • Groundwater moves by twisting and turning through interconnected small openings. • The groundwater moves more slowly when the pore spaces are smaller. Distribution and Movement of Water Underground 6.3 Water Beneath the Surface
28. Movement • Porosity • Permeability - The percentage of pore spaces - Determines how much groundwater can be stored - Ability to transmit water through connected pore spaces - Aquifers are permeable rock layers or sediments that transmit groundwater freely Distribution and Movement of Water Underground 6.3 Water Beneath the Surface
30. A spring forms whenever the water table intersects the ground surface. • Intermittent hot springs Hot Springs Geysers • Water is 6–9ºC warmer than the mean air temperature of the locality. • Water is heated by cooling of igneous rock. • Water turns to steam and erupts. Springs 6.3 Water Beneath the Surface
32. A well is a hole bored into the zone of saturation. • An artesian well is any formation in which groundwater rises on its own under pressure. • Pumping can cause a drawdown (lowering) of the water table. • Pumping can form a cone of depression in the water table. Wells 6.3 Water Beneath the Surface
34. Overuse and contamination threatens groundwater supplies in some areas. • Treating it as a nonrenewable resource • Land subsidence caused by its withdrawal • Contamination Environmental Problems Associated with Groundwater 6.3 Water Beneath the Surface
36. Erosion forms most caverns at or below the water table in the zone of saturation. A cavern is a naturally formed underground chamber. Travertine is a form of limestone that is deposited by hot springs or as a cave deposit. Caverns 6.3 Water Beneath the Surface
38. Characteristics of f eatures found within caverns • Formed in the zone of aeration • Composed of dripstone • Formed from calcite deposited as dripping water evaporates • Common features include stalactites (hanging from the ceiling) and stalagmites (growing upward from the floor ). Caverns 6.3 Water Beneath the Surface
39. Formed by dissolving rock at, or near, Earth's surface • Sinkholes —surface depressions - Sinkholes form when bedrock dissolves and caverns collapse. • Caves and caverns Common features Area lacks good surface drainage. Karst Topography 6.3 Water Beneath the Surface