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Udden grade scale

A logarithmic grade scale devised by Johan A. Udden (1859-1932), U.S.
geologist; it uses 1 mm as the reference point and progresses by the fixed
ratio of 1:2 in the direction of decreasing size and of 2:1 in the
direction of increasing size, such as 0.25, 0.5, 1, 2, 4.
See also:Wentworth grade scale

ugrandite

The group of calcium garnets uvarovite, grossular, andradite, goldmanite,
hibschite, kimzeyite, and schorlomite

uhligite

An isometric mineral, (Ca,Ti,Al,Zr)2 O3 ; forms black
octahedra in a nepheline syenite near Lake Magad, Tanzania.

uigite

A discredited term equal to thomsonite. Am. Mineral., 1

uintaite

A variety of natural asphalt occurring in the Uinta Valley, Utah, as
rounded masses of brilliant black solid hydrocarbon. Syn:gilsonite;
mineral rubber. CMD

ulexite

A triclinic mineral, NaCaB5 O6 (OH)6 .5H2 O ;
soft; forms silky white, saline crusts and masses of extremely fine
acicular crystals; in saline lake deposits as in Nevada and Chile. Also
called cotton ball; boronatrocalcite; natronborocalcite; natroborocalcite.

ullmannite

A triclinic mineral, NiSbS ; cobaltite group; pseudocubic; metallic;
steel-gray to silver-white; in veins; a source of nickel. Also called
nickel-antimony glance.

Ullrich magnetic separators

These machines have powerful electromagnets in a wedge section. The
material is treated on rolls on which magnetism is induced; they consist
of alternate disks of soft iron and some nonmagnetic material. The ore is
fed over the first roll, which removes the most magnetic material, and the
tailings go on to the second, which is weaker, where a second separation
is made. Liddell

ulmain

A kind of euvitrain that consists completely of ulmin but that is not
precipitated from solution. CF:collain

ulmification

The process of peat formation. Tomkeieff

ulmin brown

See:Vandyke brown

ulminite

a. A maceral of brown coal within the huminite group, consisting of
gelified plant-cell walls (ICCP, 1971). AGI
b. A variety of euvitrinite characteristic of ulmain and consisting of
gelified but not precipitated plant material. CF:collinite

ulrichite

A hypabyssal rock composed essentially of large phenocrysts of alkalic
feldspar, sodic pyroxene, amphibole, and nepheline with smaller
phenocrysts of accessory olivine. Feldspar, pyroxene, and amphibole recur
in the groundmass. A porphyritic variety of olivine-bearing phonolite.
Syn:uraninite

ultimate analysis

a. The determination of the elements contained in a compound, as
distinguished from proximate analysis, which is the determination of the
compounds contained in a mixture. Standard, 2
b. In the case of coal and coke, the determination of carbon and hydrogen
in the material, as found in the gaseous products of its complete
combustion, the determinations of sulfur, nitrogen, and ash in the
material as a whole, and the calculation of oxygen by difference.
ASTM
c. The principal reason for the ultimate analysis of coal is for the
classification of coals according to rank, although it is often used for
commercial and industrial purposes when it is most desirable to know the
sulfur content of coal. Also known as total analysis of coal.
Cooper

ultimate bearing capacity

The average load per unit of area required to produce failure by rupture
of a supporting soil mass. See also:bearing capacity

ultimate bearing pressure

The pressure under which a foundation will settle with no increase of
load. See also:plate bearing test

ultimate CO2

The percent of carbon dioxide that would appear in the flue gases if
combustion were perfect. Varies with the fuel. Strock, 2

ultimate compressive strength

That point at which failure by crushing occurs. Pryor, 3

ultimate elongation

The percentage of permanent deformation remaining after tensile rupture,
measured over an arbitrary length including the section of rupture.
Roark

ultimately controlled variable

In mineral processing, the variable whose control is the end purpose of
the automatic control system. Fuerstenau

ultimate strength

The ultimate strength of a material in tension, compression, or shear,
respectively, is the maximum tensile, compressive, or shear stress that
the material can sustain, calculated on the basis of the ultimate load and
the original or unstrained dimensions. It is implied that the condition of
stress represents uniaxial tension, uniaxial compression, or pure shear,
as the case may be. Roark