Lyman James Briggs (May 7, 1874 – March 25, 1963) was an American engineer, physicist and administrator. He was the third director of the National Bureau of Standards (NBS) during the Great Depression and chairman of the Uranium Committee before America entered the Second World War. The Lyman Briggs College at Michigan State University is named in his honor.
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In this Dossier
- ⭐ Core Definition: Lyman Briggs
- Lyman Briggs in the context of Field capacity
- Lyman Briggs in the context of Moisture equivalent
Lyman Briggs in the context of Field capacity
Field capacity is the amount of soil moisture or water content held in the soil after excess water has drained away and the rate of downward movement has decreased. This usually occurs two to three days after rain or irrigation in pervious soils of uniform structure and texture. The nominal definition of field capacity (expressed symbolically as θfc) is the bulk water content retained in soil at −33 kPa (or −0.33 bar) of hydraulic head or suction pressure. The term originated from Israelsen and West and Frank Veihmeyer and Arthur Hendrickson.
Veihmeyer and Hendrickson realized the limitation in this measurement and commented that it is affected by so many factors that, precisely, it is not a constant (for a particular soil), yet it does serve as a practical measure of soil water-holding capacity. Field capacity improves on the concept of moisture equivalent by Lyman Briggs. Veihmeyer & Hendrickson proposed this concept as an attempt to improve water-use efficiency for farmers in California in 1949.
View the full Wikipedia page for Field capacityLyman Briggs in the context of Moisture equivalent
Moisture equivalent is proposed by Lyman Briggs and McLane (1910) as a measure of field capacity for fine-textured soil materials. Moisture equivalent is defined as the percentage of water which a soil can retain in opposition to a centrifugal force 1000 times that of gravity. It is measured by saturating sample of soil 1 cm thick, and subjecting it to a centrifugal force of 1000 times gravity for 30 min. The gravimetric water content after this treatment is its moisture equivalent.This concept is no longer used in soil physics and has been replaced by field capacity.
Lyman Briggs and Homer LeRoy Shantz (1912) found that:
View the full Wikipedia page for Moisture equivalent