A Microprocessor Based Magnetic Tape Drive Interface

1986 ◽  
Vol 3 (1) ◽  
pp. 26-28 ◽  
Author(s):  
Eurico J. D'Sa
Keyword(s):  
1986 ◽  
Vol 108 (1) ◽  
pp. 22-28 ◽  
Author(s):  
B. Bhushan ◽  
G. W. Nelson ◽  
M. E. Wacks

The transfer of wear debris of a nickel-zinc ferrite head to a magnetic tape was measured by autoradiography of the tape after it was worn against the irradiated ferrite head. Ferrite deposits on the tape were observed only after 5000 passes. Dots or specks on the autoradiograph of the tapes of about 200 micrometers in diameter, caused by particles of ferrite about 1 μm in diameter and mass of about 10−11 g, were measured. The average amount of ferrite deposited on the tape after 20,000 passes was about 0.6 nanogram per square centimeter; some areas showed uniform deposits of ferrite concentration of 10–20 ng/cm2. Based on our estimates of total head wear, only a small fraction (about 0.6 percent) of the total ferrite wear debris was transferred to the tape, about 0.2 percent was transferred to the tape-drive component surfaces, and the rest, we conclude, was airborne.


1985 ◽  
Vol 21 (5) ◽  
pp. 1560-1562 ◽  
Author(s):  
D. O'Connor ◽  
F. Shelledy ◽  
D. Heim

1974 ◽  
Vol 10 (3) ◽  
pp. 892-894 ◽  
Author(s):  
H. Fraser ◽  
F. Hauke ◽  
G. Lammers ◽  
T. Wise

Wear ◽  
2003 ◽  
Vol 255 (7-12) ◽  
pp. 1323-1333 ◽  
Author(s):  
Bharat Bhushan ◽  
Paritosh P Ambekar

2008 ◽  
Vol 131 (1) ◽  
Author(s):  
Bart Raeymaekers ◽  
Frank E. Talke

The sources of lateral tape motion in a tape drive are reviewed. Currently used measurement methods and models for lateral tape motion are analyzed and compared. The effect of roller run-out, tape edge contact, and tape tension transients on lateral tape motion is discussed. A dual stage actuator tape head is investigated to improve track-following capability and increase the track density on a magnetic tape.


1991 ◽  
Vol 81 (4) ◽  
pp. 1380-1390
Author(s):  
K. R. Gledhill ◽  
M. J. Randall ◽  
M. P. Chadwick

Abstract An earthquake detection and recording system known as EARSS has been developed for permanent seismograph stations and temporary field installations. It records three components of ground motion with a dynamic range of 120 dB. A frequency-domain algorithm detects earthquakes and initiates the recording of data on magnetic tape. Alternatively, EARSS can record data continuously, for preselected periods of time, or recording can be triggered by a time-domain phase picker. Up to 1500 earthquakes (25.5 Mbytes) can be recorded on each magnetic tape cartridge. The field version of EARSS supplies power to the tape drive only when data is being written to tape, thus reducing the normal power consumption of 12 watts (at 12 volts) to 2.5 watts. A field trial using a network of eight EARSS seismographs resulted in 1020 successful station-days of operation from a possible total of 1098 station-days (3 years). Of the 78 lost days of operation, 23 were due to power supply problems external to EARSS, and 52 were caused by a low-temperature failure of the recording system, which has since been corrected. A total of 442 Mbytes of data were recorded, of which about 250 Mbytes were useful data.


2014 ◽  
Vol 556 ◽  
pp. 354-360 ◽  
Author(s):  
Ehsan Rismani ◽  
Reuben Yeo ◽  
Hamed Mirabolghasemi ◽  
Wee Ming Kwek ◽  
Hyunsoo Yang ◽  
...  

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