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Solutions for Chapter 1.5: Ideal Gas Law
Full solutions for Fundamentals of Fluid Mechanics | 8th Edition
The force exerted by the weight of a column of air above a given point.
Andean-type plate margin
Plate boundaries that generate continental volcanic arcs.
An amphitheater-shaped basin at the head of a glaciated valley produced by frost wedging and plucking.
A system that is self-contained with regards to matter—that is, no matter enters or leaves.
A star that varies in brightness.
Small earthquakes that often precede a major earthquake.
A short wall built at a right angle to the shore to trap moving sand.
Humid subtropical climate
A climate generally located on the eastern side of a continent and characterized by hot, sultry summers and cool winters.
The height to which convectional movements extend above Earth’s surface. The greater the mixing depth, the better the air quality.
The theory that proposes that Earth’s outer shell consists of individual plates that interact in various ways and thereby produce earthquakes, volcanoes, mountains, and the crust itself.
A lake formed during a period of increased rainfall. During the Pleistocene epoch this occurred in some nonglaciated regions during periods of ice advance elsewhere.
A device consisting of two thermometers (wet bulb and dry bulb) that is rapidly whirled and, with the use of tables, yields the relative humidity and dew point.
A telescope designed to make observations in radio wavelengths.
Transportation of sediment through a series of leaps or bounces.
Seaward of the coast, this zone extends from the highest level of wave action during storms to the lowest tide level.
A soil classification system consisting of six hierarchical categories based on observable soil characteristics. The system recognizes 12 soil orders.
A situation in which the surface position of a front does not move; the flow on either side of such a boundary is nearly parallel to the position of the front.
One of the three main categories of meteorites. Such meteorites are composed largely of silicate minerals with inclusions of other minerals.
An opening bored into the zone of saturation.