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See also:INCLINOMETER (See also:Dip CIRCLE) . Two distinct classes of See also:instruments are used for measuring the dip (see See also:MAGNETISM, TERRESTRIAL) or inclination of the See also:earth's magnetic See also: There are also two adjustable stops which can be set in any position, and allow the upper See also:part of the See also:instrument to be rotated through exactly 1800 without the See also:necessity of reading the horizontal circle. When making a determination of the dip with the dip circle, a number of See also:separate readings have to be made in See also:order to eliminate various instrumental defects. Thus, that side of the needle on which the number is engraved being called the See also:face of the needle, and that side of the protecting box next the vertical circle the face of the instrument, both ends of the needle are observed in the following relative positions, the instrument being in every case so adjusted in azimuth that the axle of the needle points magnetic See also:east and See also:west: i. Face of instrument east and face of needle next to face of instrument; ii. Face of instrument west and face of needle next to face of instrument; iii. Face of instrument west and face of needle away from face of instrument; iv. Face of instrument east and face of needle away from face of instrument. Next the direction of magnetization of the needle is reversed by stroking it a number of times with two strong permanent magnets, when the other end of the needle dips and the above four sets of readings are repeated. The See also:object in reading both ends of the needle is to avoid See also:error if the prolongation of the axle of the needle does not pass through the centre of the vertical circle, as also to avoid error due to the eccentricity of the arm which carries the reading microscopes and verniers. The reversal of the instrument between (i.) and (ii.) and between (iii.) and (iv.) is to eliminate errors due to (a) the See also:line joining the zeros of the vertical circle not being exactly horizontal, and (b) the agate knife-edges which support the needle not being exactly horizontal. The reversal of the needle between (ii.) and (iii.) is to eliminate errors due to (a) the magnetic axis of the needle not coinciding with the line joining the two points of the needle, and (h) to the centre of gravity of the needle being displaced from the centre of the axle in a direction at right angles to the length of the needle. The reversal of the poles of the needle is to counteract any error produced by the centre of gravity of the needle being displaced from the centre of the axle in a direction parallel to the length of the needle. For use at See also:sea the dip circle was modified by See also:Robert Were See also:Fox (See also:Annals of See also:Electricity, 1839, 3, p. 288), who used a needle having pointed axles, the points resting in jewelled holes carried by two uprights, so that the See also:movement of the See also:ship does not cause the axle of the needle to See also:change its position with reference to the vertical divided circle. To counteract the tendency of the axle to stick in the See also:bearings, the instrument is fitted with a knob on the See also:top of the box protecting the needle, and when a reading is being taken this knob is rubbed with an See also:ivory or See also:horn disk, the See also:surface of which is corrugated. In this way a tremor is caused which is found to assist the needle in overcoming the effects of See also:friction, so that it takes up its true position. In the Creak modification of the Fox dip circle, the upper halves of the jewels which See also:form the bearings are cut away so that the needle can be easily removed, and thus the reversals necessary when making a See also:complete observation can be performed (see also MAGNETO-See also:METER). Induction Inclinometers.—The principle on which induction inclinometers depend is that if a coil of insulated See also:wire is spun about a diameter there will be an alternating current induced in the coil, unless the axis about which it turns is parallel to the lines of force of the earth's field. Hence if the axis about which such a coil spins is adjusted till a sensitive See also:galvanometer connected to the coil through a commutator, by which the alternating current is converted into a See also:direct current, is undeflected, then the axis must be parallel to the lines of force of the earth's field, and hence the inclination of the axis to the horizontal is the dip. The introduction and perfection of this type of inclinometeris almost entirely due to H. See also:Wild. His form of instrument for field observations' consists of a coil ro cm. in diameter, containing about See also:rood turns of See also:silk-covered See also:copper wire, the resistance being about 40 ohms, which is pivoted inside a See also:metal See also:ring. This ring can itself rotate about a horizontal axle in its own See also:plane, this axle being at right angles to that about which the coil can rotate. Attached to the axle of the ring is a divided circle, by means of which and two reading microscopes the inclination of the axis of rotation of the coil to the horizontal can be read. The bearings which support the horizontal axle of the ring are mounted on a horizontal annulus which can be rotated in a groove attached to the See also:base of the instrument, as so to allow the azimuth of the axle of the ring, and hence also that of the plane in which the axis of the coil can move, to be adjusted. The coil is rotated by means of a flexible See also:shaft worked by a small cranked handle and a See also:train of See also:gear wheels. The terminals of the coil are taken to a two-part commutator of the See also:ordinary See also:pattern on which See also:rest two copper brushes which are connected by flexible leads to a sensitive galvanometer. The inclination of the axis of the coil can be roughly adjusted by See also:hand by rotating the supporting ring. The final See also:adjustment is made by means of a See also:micrometer See also:screw attached to an arm which is clamped on the axle of the ring. When making a measurement the azimuth circle is first set horizontal, a striding level placed on the trunnions which carry the ring being used to indicate when the adjustment is complete. The striding level is then placed on the axle which carries the coil, and when the bubble is at the centre of the See also:scale the micro-scopes are adjusted to the zeros of the vertical circle. A box containing a long See also:compass needle and having two feet with inverted V's is placed to rest on the axle of the coil, and the instrument is turned in azimuth till the compass needle points to a lubber line on the box. By this means the axis of the coil is brought into the magnetic See also:meridian. The commutator being connected to a sensitive galvanometer, the coil is rotated, and the ring adjusted till the galvanometer is undeflected. The reading on the vertical. circle then gives the dip. By a See also:system of reversals slight faults in the adjustment of the instrument can be eliminated as in the case of the dip circle. With such an instrument it is claimed that readings of dip can be made accurate to o•1 minutes of arc.
The form of Wild inductor for use in a fixed See also:observatory differs from the above in that the coil consists of a See also:drum-See also:wound See also:armature, but without See also:iron, of which the length is about three times the diameter. This armature has its axle mounted in a See also:frame attached to the sloping side of a See also: Zeits. (1895), 12, p. 41. Additional information and CommentsThere are no comments yet for this article.
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