MLchartDataset catalogue

Groundwater flow

Term · Meteorology and atmospheric science · MLC-T-MET-006108

The movement of water beneath the Earth's surface through saturated zones within soil and rock. This flow is driven by gravity and pressure differences, moving from areas of higher hydraulic head to lower hydraulic head. Groundwater flow rates are influenced by the permeability of the geological material and the hydraulic gradient, typically measured in meters per day or per year.

Table 1. Record
IdentifierMLC-T-MET-006108
FieldMeteorology and atmospheric science
Record as JSON
{
  "id": "MLC-T-MET-006108",
  "term": "Groundwater flow",
  "field": "Meteorology and atmospheric science",
  "definition": "The movement of water beneath the Earth's surface through saturated zones within soil and rock. This flow is driven by gravity and pressure differences, moving from areas of higher hydraulic head to lower hydraulic head. Groundwater flow rates are influenced by the permeability of the geological material and the hydraulic gradient, typically measured in meters per day or per year.",
  "url": "https://mlchart.com/terminology/meteorology/groundwater-flow/"
}

Record 4,319 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.