Assertion: aquifer's transmissivity | /r/HasProperty | squared per day
Facets:
value: in these areas
type: LOCATION
value: generally
type: DEGREE
value: over much
type: DEGREE
Source sentences:
text: The transmissivity of the Laramie-Fox Hills aquifer, for example, is less than 5 feet squared per day near the northwestern margin of the aquifer and is less than 100 feet squared per day over much of the remaining area.
text: The transmissivity of the Laramie-Fox Hills aquifer, for example, is less than 5 feet squared per day near the northwestern margin of the aquifer and is less than 100 feet squared per day over much of the remaining area.
text: The determined transmissivity throughout most of the confined freshwater aquifer ranges from 430,000 to 2,200,000 feet squared per day; the determined transmissivity of the unconfined aquifer generally is less than 430,000 feet squared per day.
text: The mean estimated transmissivity of the Piney Point aquifer in York and James City Counties is 16,300 feet squared per day (ft2/d), but farther north it is only 925 ft2/d.
text: In these areas, transmissivity is more than 13,000 feet squared per day generally and locally exceeds 27,000 feet squared per day.
text: The High Plains aquifer in eastern Colorado and eastern New Mexico has an average saturated thickness of about 75 feet; the average transmissivity of the aquifer is about 4,500 feet squared per day.
text: Working with a minimal dataset in Webb County (four measurements), Mace and others (2000) estimated the average transmissivity of the Carrizo-Wilcox aquifer in Webb County to be 69 feet squared per day (ft2/d).
text: All of the area having a transmissivity greater than 1,000,000 feet squared per day and most of the area having transmissivity from 250,000 to 1,000,000 feet squared per day are where the upper confining unit of the Floridan aquifer system is less than 100 feet thick, or is absent (compare figs.