Throughflow is the tranfer of water through th soil. Surface runoff is the transfer of water where the soil is impermeable so the transfer of water is on top of the soil.
According to Wikipedia, throughflow is "the movement of water horizontally beneath the land surface". Water permeates through the soil's surface, gravity draws it downwards, and continues to flow until it reaches an underground river or lake. Another definition of throughflow is the Indonesian Throughflow, an ocean current that transports water between the Pacific Ocean and the Indian Ocean through the Indonesian Archipelago.
Surface runoff refers to water that flows over the land surface and collects in rivers, lakes, and oceans. Groundwater flow, on the other hand, is water that moves underground through porous rock and soil materials. Surface runoff is influenced by factors such as precipitation and topography, while groundwater flow is influenced by geological formations and groundwater levels.
Through flow in the water cycle refers to the horizontal movement of water through soil and rock layers. It occurs when precipitation infiltrates the ground and moves laterally before reaching a body of water like a river or lake. Through flow plays a crucial role in groundwater recharge and the overall movement of water within watersheds.
difference between laminar air flow & reverse laminar air flow
Groundwater would flow quickly through rocks with high porosity and high permeability. These characteristics allow for water to flow easily through the spaces between the rock particles with minimal obstructions, resulting in fast rates of groundwater movement.
Base flow is the portion of streamflow that comes from groundwater discharge, but it is not exactly the same as groundwater. Groundwater refers to the water stored underground in aquifers, while base flow specifically refers to the contribution of groundwater to streamflow during dry periods when surface runoff is low.
C. J. Haefeli has written: 'Regional groundwater flow between Lake Simcoe and Lake Ontario' -- subject(s): Groundwater
The flow of groundwater is an aquifer.
Porosity and permeability of rocks and soil determine how much water can be stored and how easily it can flow through groundwater. Rocks like sandstone and limestone with high porosity and permeability are good at storing and allowing the movement of groundwater. Conversely, impermeable rocks like clay or granite store less water and restrict the flow of groundwater.
what's the difference between flow chart and structure diagrams and pseudo code
Groundwater flow.