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関連する概念動画

Gradually Varying Flow01:29

Gradually Varying Flow

Gradually varying flow (GVF) in open channels describes situations where water depth changes slowly along the channel due to factors like non-uniform bed slope, channel shape variations, or obstructions. This flow type occurs when the depth adjusts gradually to balance gravitational forces, shear forces, and energy requirements, resulting in a low rate of depth change.Characteristics of Gradually Varying FlowGVF is commonly observed in natural streams, rivers, and canals, where flow depth...
Underflow Gates01:30

Underflow Gates

Underflow gates are vital for controlling water flow in irrigation canals. The three main types of underflow gates — vertical, radial, and drum gates — serve different purposes while ensuring effective flow management. Vertical gates move up and down, generating a free-flowing water jet; radial gates pivot to regulate the flow; and drum gates rotate for precise adjustments. The flow through these gates is influenced by downstream conditions, resulting in free or drowned outflow.Free and Drowned...
The Water Cycle01:00

The Water Cycle

The Earth’s hydrosphere includes all of the areas where the storage and movement of water occurs. Since water is the basis of all living processes, the cycling of water is extremely important to ecosystem dynamics.
Pressure Variation in a Fluid at Rest01:11

Pressure Variation in a Fluid at Rest

In a fluid at rest, the pressure at any point beneath the fluid surface depends solely on the depth, not on the container's shape or size. This principle, known as hydrostatic pressure, arises because, in stationary fluids, there is no acceleration, meaning the forces within the fluid balance out. Only vertical forces, caused by the weight of the fluid above, contribute to pressure changes with depth.
When measuring pressure at two different levels within the fluid, the difference in pressure...
Precipitation Gravimetry01:03

Precipitation Gravimetry

Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
Plane Potential Flows01:23

Plane Potential Flows

Plane potential flows simplify fluid motion by assuming the fluid to be irrotational and incompressible. These characteristics allow these flows to be described by a velocity potential function, ϕ, representing the flow speed in a given direction, and a stream function, ψ, that visualizes the flow path, both governed by Laplace's equation. These parameters help in estimating flow patterns, velocity distributions, and pressure fields around various hydraulic structures.
Uniform Flow
Uniform flow...

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関連する実験動画

Updated: May 14, 2026

Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
08:09

Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management

Published on: September 12, 2017

地下水表の深さのグローバルパターン

Y Fan1, H Li, G Miguez-Macho

  • 1Department of Earth and Planetary Sciences, Rutgers University, New Brunswick, NJ 08854, USA. yingfan@rci.rutgers.edu

Science (New York, N.Y.)
|February 23, 2013
PubMed
まとめ

浅い地下水は,世界の陸地生態系にとって不可欠であり,陸地の22-32%を支えている. 水表の深さを理解することは,生態系の健康と水資源管理の鍵です.

科学分野:

  • 地球科学 地球科学 地球科学
  • エコロジー エコロジー エコロジー
  • 水文学 水文学とは,水文学の学問である.

背景:

  • 浅い地下水は,河川の底流と根帯の土壌水分を維持することによって,陸上の生態系を維持します.
  • 地表水深のグローバルパターンとその生態学的意義は,依然として十分に理解されていない.

研究 の 目的:

  • 世界的な水表の深さのパターンをマッピングするために.
  • 浅い地下水が陸上生態系を重要に支える地域を特定する.

主な方法:

  • 政府のアーカイブと文献から集めた,世界の水表の深さの観測をまとめました.
  • 気候,地形,海面データを駆動した地下水モデルを利用してパターンを推測し,データギャップを埋める.

主要な成果:

  • 浅い地下水は,世界の土地面積の22~32%に影響を与えています.
  • 陸地の約15%には地下水で満たされる地表水があり,7~17%には植物の根深さの範囲内に地下水がある.
  • 地表水深のパターンは,世界の湿地分布と地域/地方の植生グラデーションと相関しています.

結論:

  • 浅い地下水は,地球上の陸上生態系を支える上で重要な役割を果たしています.

さらに関連する動画

Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar
07:14

Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar

Published on: May 1, 2018

Continuous Hydrologic and Water Quality Monitoring of Vernal Ponds
06:37

Continuous Hydrologic and Water Quality Monitoring of Vernal Ponds

Published on: November 13, 2017

関連する実験動画

Last Updated: May 14, 2026

Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
08:09

Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management

Published on: September 12, 2017

Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar
07:14

Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar

Published on: May 1, 2018

Continuous Hydrologic and Water Quality Monitoring of Vernal Ponds
06:37

Continuous Hydrologic and Water Quality Monitoring of Vernal Ponds

Published on: November 13, 2017

  • 地表水深のマッピングは,生態系の機能と水資源の利用可能性を理解するために不可欠です.