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Groundwater is water located beneath the Earth's surface in porous rock and sediment. It originates from rainfall and snowmelt that filters underground, and eventually makes its way back above ground in streams, lakes, and oceans. Groundwater accounts for 1% of the water on Earth but makes up 35 times more than surface water in lakes and streams. It occurs everywhere but is usually found within 750 meters of the surface, and there is enough groundwater to cover the entire Earth's surface in a 55-meter thick layer.
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Presentation1.pptx
Groundwater is water located beneath the Earth's surface in soil and rock pores and fractures. It originates from rainfall and snowmelt that infiltrates underground, where it flows slowly through aquifers before emerging in streams, lakes, or oceans. Groundwater makes up about 1% of the Earth's total water but over 35 times the amount found in surface water bodies. It is usually found within 750 meters of the surface and globally amounts to a 55-meter thick layer spread across the planet. Groundwater occurs via properties like porosity, permeability, and in aquifers - geologic formations that can store and transport water economically. Its origins are primarily recent meteoric water from rainfall infiltration or ancient "fossil water
Water.ppt.pptx
Groundwater originates as rainfall or snowmelt that seeps into the ground and fills pore spaces and fractures in rocks and sediments below the Earth's surface. It makes up about 1% of the water on Earth but over 35 times as much water as is contained in all lakes and streams. Groundwater occurs nearly everywhere and generally to depths less than around 750 meters. The global volume of groundwater is equivalent to a 55-meter thick layer spread over the entire planet. The occurrence and flow of groundwater is influenced by factors such as topography, climate, geology, and the properties of underground materials. There are four main sources of groundwater: connate water trapped during rock formation, rainfall, irrigation water, and tidal
Chapter 1 occurrence of groundwater
Groundwater occurs beneath the Earth's surface in pore spaces and fractures in rocks and sediments. It originates from rainfall and snowmelt percolating into the ground. Groundwater is found everywhere but is usually within 750 meters of the surface. It makes up about 1% of the total water on Earth but 35 times the amount of water in streams and lakes. Groundwater flows through the hydrologic cycle, entering the ground as precipitation and eventually emerging in streams, lakes, or oceans.
Reportinscience bautista-regala
This is our group work in our science subject. We are assigned to make a power point presentation in order for us to understand and share our knowledge in the given chapter. We hope that you learned from the presentation the we have presented, thank you and good luck!
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The document discusses the water cycle and its key processes. It describes how water evaporates from surfaces due to heat from the sun, condenses to form clouds, precipitates as rain, snow or hail, and either runs off on the surface or infiltrates into the ground to replenish groundwater stores or be absorbed by plant roots through transpiration. It then focuses on groundwater, describing it as water residing in saturated underground areas, and how it is stored in aquifers. It identifies sewage as a major cause of groundwater pollution.
Eath sci (compuesto, dimabayao)
Water exists in four main spheres on Earth and cycles between them through evaporation and precipitation. It covers 71% of the planet's surface. The hydrologic cycle describes the continuous movement of water between the atmosphere, land, and oceans through various processes. This includes evaporation, transpiration, condensation, precipitation, and runoff. Water is essential but threats like pollution, overuse, and climate change increase pressures on this critical resource that requires wise management.
Gonzales trajico report (chapter4)
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Presentation1.pptx
Groundwater is water located beneath the Earth's surface in soil and rock pores and fractures. It originates from rainfall and snowmelt that infiltrates underground, where it flows slowly through aquifers before emerging in streams, lakes, or oceans. Groundwater makes up about 1% of the Earth's total water but over 35 times the amount found in surface water bodies. It is usually found within 750 meters of the surface and globally amounts to a 55-meter thick layer spread across the planet. Groundwater occurs via properties like porosity, permeability, and in aquifers - geologic formations that can store and transport water economically. Its origins are primarily recent meteoric water from rainfall infiltration or ancient "fossil water
Water.ppt.pptx
Groundwater originates as rainfall or snowmelt that seeps into the ground and fills pore spaces and fractures in rocks and sediments below the Earth's surface. It makes up about 1% of the water on Earth but over 35 times as much water as is contained in all lakes and streams. Groundwater occurs nearly everywhere and generally to depths less than around 750 meters. The global volume of groundwater is equivalent to a 55-meter thick layer spread over the entire planet. The occurrence and flow of groundwater is influenced by factors such as topography, climate, geology, and the properties of underground materials. There are four main sources of groundwater: connate water trapped during rock formation, rainfall, irrigation water, and tidal
Chapter 1 occurrence of groundwater
Groundwater occurs beneath the Earth's surface in pore spaces and fractures in rocks and sediments. It originates from rainfall and snowmelt percolating into the ground. Groundwater is found everywhere but is usually within 750 meters of the surface. It makes up about 1% of the total water on Earth but 35 times the amount of water in streams and lakes. Groundwater flows through the hydrologic cycle, entering the ground as precipitation and eventually emerging in streams, lakes, or oceans.
Reportinscience bautista-regala
This is our group work in our science subject. We are assigned to make a power point presentation in order for us to understand and share our knowledge in the given chapter. We hope that you learned from the presentation the we have presented, thank you and good luck!
Fresh water
The document discusses the water cycle and its key processes. It describes how water evaporates from surfaces due to heat from the sun, condenses to form clouds, precipitates as rain, snow or hail, and either runs off on the surface or infiltrates into the ground to replenish groundwater stores or be absorbed by plant roots through transpiration. It then focuses on groundwater, describing it as water residing in saturated underground areas, and how it is stored in aquifers. It identifies sewage as a major cause of groundwater pollution.
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Water exists in four main spheres on Earth and cycles between them through evaporation and precipitation. It covers 71% of the planet's surface. The hydrologic cycle describes the continuous movement of water between the atmosphere, land, and oceans through various processes. This includes evaporation, transpiration, condensation, precipitation, and runoff. Water is essential but threats like pollution, overuse, and climate change increase pressures on this critical resource that requires wise management.
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Water is essential for life on Earth and is continuously circulated through various reservoirs in the hydrosphere in a process known as the water cycle. The water cycle involves evaporation of water from oceans, rivers and lakes into vapor which rises into the atmosphere. Water vapor condenses to form clouds and precipitation falls back to the Earth's surface, completing the cycle. Most of Earth's water is saline and located in oceans, while freshwater is found in ice sheets, groundwater, atmosphere and other reservoirs with varying residence times.
Hydrology
The water cycle describes the continuous movement of water on, above and below the Earth's surface through various physical processes. Water evaporates from oceans, lakes, and vegetation into the atmosphere. It condenses to form clouds and precipitates as rain or snow. Precipitation may fall directly into water bodies, be intercepted by plants, infiltrate soils, or become surface runoff into streams, contributing to the total streamflow or base flow. Water is stored temporarily in the atmosphere, oceans, lakes, soils, aquifers and glaciers before repeating the cycle.
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ground water
Groundwater is water found below the Earth's surface. It occupies pore spaces in rocks and soil. There are three main types of aquifers - confined, unconfined, and semi-confined. Confined aquifers are bounded above and below by layers of rock that do not allow water to move through them easily. Unconfined aquifers have a layer of permeable rock or soil at the top that allows water to recharge. Semi-confined aquifers have a layer of low permeability at the top. Important properties of aquifers include porosity, specific yield, hydraulic conductivity, and the type and permeability of the rock material.
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Hydro1
The hydrologic cycle describes the continuous movement of water on, above, and below the surface of the Earth. The three main stages are evaporation, transpiration, and precipitation. Evaporation and transpiration move water from oceans and plants into the atmosphere, where water vapor condenses and falls as precipitation. Precipitation provides the primary mechanism for delivering atmospheric water to the Earth's surface, where it runs off into streams and rivers or infiltrates into soils and groundwater. The hydrologic cycle is powered by energy from the sun and is crucial for sustaining life on Earth.
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The complex relationship between human activities and the environment has been the focus
of extensive research and worry. As the global community grapples with swift urbanization,
population expansion, and economic progress, the effects on natural ecosystems are becoming
more evident. A crucial element of this impact is the alteration of vegetation cover, which plays a
significant role in maintaining the ecological equilibrium of our planet.Land serves as the foundation for all human activities and provides the necessary materials for
these activities. As the most crucial natural resource, its utilization by humans results in different
'Land uses,' which are determined by both human activities and the physical characteristics of the
land.
The utilization of land is impacted by human needs and environmental factors. In countries
like India, rapid population growth and the emphasis on extensive resource exploitation can lead
to significant land degradation, adversely affecting the region's land cover.
Therefore, human intervention has significantly influenced land use patterns over many
centuries, evolving its structure over time and space. In the present era, these changes have
accelerated due to factors such as agriculture and urbanization. Information regarding land use and
cover is essential for various planning and management tasks related to the Earth's surface,
providing crucial environmental data for scientific, resource management, policy purposes, and
diverse human activities.
Accurate understanding of land use and cover is imperative for the development planning
of any area. Consequently, a wide range of professionals, including earth system scientists, land
and water managers, and urban planners, are interested in obtaining data on land use and cover
changes, conversion trends, and other related patterns. The spatial dimensions of land use and
cover support policymakers and scientists in making well-informed decisions, as alterations in
these patterns indicate shifts in economic and social conditions. Monitoring such changes with the
help of Advanced technologies like Remote Sensing and Geographic Information Systems is
crucial for coordinated efforts across different administrative levels. Advanced technologies like
Remote Sensing and Geographic Information Systems
9
Changes in vegetation cover refer to variations in the distribution, composition, and overall
structure of plant communities across different temporal and spatial scales. These changes can
occur natural.
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slide pre.pptx
- 1. Aquifer, which is a geologic formation sufficiently porous to store water and permeable enough to allow water to flow through them in economic quantities. Storage coefficient, which is the volume of water that an aquifer releases from or takes into storage per unit surface area of aquifer per unit change in the component of area normal to surface.
- 2. GROUNDWATER Introduction Groundwater is water that exists in the pore spaces and fractures in rocks and sediments beneath the Earth’s surface. It originates as rainfall or snow, and then moves through the soil and rock into the groundwater system, where it eventually makes its way back to the surface streams, lakes, or oceans. Groundwater makes up about 1% of the water on the Earth (most water is in oceans)
- 3. To understand the ways in which groundwater occurs, it is needed to think about the ground and the water properties. Porosity, which is the property of a rock possessing pores or voids. Saturated and unsaturated zones. Permeability, which is the ease with which water can flow through the rock.
- 4. Origin of Groundwater The origin of groundwater is primarily one of the following: Groundwater derived from rainfall and infiltration within the normal hydrological cycle. This kind of water is called meteoric water. The name implies recent contact with the atmosphere. Fossil water if fresh may be originated from the fact of climate change phenomenon, i.e., some areas used to have wet weather and the aquifers of that area were recharged and then the weather of that area becomes dry.
- 5. Introduction Cont. But, groundwater makes up to 35 times the amount of water in lakes and streams. Groundwater occurs everywhere beneath the Earth’s surface, but is usually restricted to depth less than about 750 meters. The volume of groundwater is equivalent to a 55-meter thick layer spread out over the entire surface of the Earth