MLchartDataset catalogue

Field permeability

Term · Meteorology and atmospheric science · MLC-T-MET-005566

The rate at which water can move through a soil or rock layer under natural conditions in the field. This property is determined by the interconnectedness of pores and fractures, influencing groundwater flow and infiltration rates. Field permeability is often measured using methods like the double-ring infiltrometer or pump tests.

Table 1. Record
IdentifierMLC-T-MET-005566
FieldMeteorology and atmospheric science
Record as JSON
{
  "id": "MLC-T-MET-005566",
  "term": "Field permeability",
  "field": "Meteorology and atmospheric science",
  "definition": "The rate at which water can move through a soil or rock layer under natural conditions in the field. This property is determined by the interconnectedness of pores and fractures, influencing groundwater flow and infiltration rates. Field permeability is often measured using methods like the double-ring infiltrometer or pump tests.",
  "url": "https://mlchart.com/terminology/meteorology/field-permeability/"
}

Record 3,519 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.