浸透 (水文学)
1. Infiltration (hydrology)Infiltration is the process by which water on the ground surface enters the soil. Infiltration rate in soil science is a measure of the rate at which soil is able to absorb rainfall or irrigation. It is measured in inches per hour or millimeters per hour. The rate decreases as the soil becomes saturated. If the precipitation rate exceeds the infiltration rate, runoff will usually occur unless there is some physical barrier.
Read “Infiltration (hydrology)” on English Wikipedia
Read “浸透 (水文学)” on Japanese Wikipedia
Read “Infiltration (hydrology)” on DBpedia
Read “Infiltration (hydrology)” on English Wikipedia
Read “浸透 (水文学)” on Japanese Wikipedia
Read “Infiltration (hydrology)” on DBpedia
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