Memory Storage Devices

--Donghyun727 (talk) 18:49, 5 December 2015 (EST)Lee Dong Hyun

Magnetic storage devices use the method of magnetic recording to preserve data.

Magnetic recording

Magnetic recording is a process where portions of a magnetic material are selectively magnetized with the use of electrical signals. The first use of this kind of technique was introduced by a Danish engineer Valdemar Poulsen in 1900. He created a machine called telegraphone that allowed him to record speech magnetically on a steel wire, and this became the start of many storage devices that are existent today.

How it works

Magnetic recording

Recording methods

Analog Recording

Analog recording was the most popular method used when tapes were the most prevalent recording devices. The tape would run at a constant speed, and the writing head magnetizes the tape in response to the signals required to record a particular piece of data. Once a magnetization distribution is completed to store the relevant data, this distribution can be read out to replay the original signal which triggered the magnetization. The commonly used magnetic particles for this method are Iron oxide particles or Chromium oxide.

Digital Recording

Digital recording can be considered a more advanced method of recording, as instead of creating a magnetization distribution, digital recording makes use of magnetic states. The method involves the usage of two stable magnetic states, which are the +Ms and the -Ms on a hysteresis loop. This is a technique which is used to create devices such as floppy disks and the currently popular hard disk drives.

Recording media on HDDs use a stack of thin films to store information and a read/write head to read and write information to and from the media; various developments have been carried out in the area of used materials.[5]

Magnetic recording consists of leaving patterns of remanent magnetization on a track within the surface of magnetic media that sits on top of a non-magnetic substrate. There are three main orientations of the magnetization with respect to the track, lateral (hardly ever used), longitudinal (the current standard), and perpendicular (Figure 2).

Figure 2:Longitudinal, perpendicular, and lateral recording.

Most common is longitudinal recording. For this type of recording, the transducer, or recording head, is a ring-shaped electromagnet with a gap at the surface facing the media. When the head is fed with a current, the fringing field from the gap magnetizes the magnetic media, as is shown in Figure 3. The media moves at constant velocity under the recording head, as is shown in Figure 1. The temporal changes in the current leave spatial variations in the remanent magnetization along the length of the track.

Figure 3: Magnetic Write Head Schematics: Functioning of the Gap

The recorded magnetization creates a pattern of magnetic fields that can be picked up be the media moving under the read head. Under ideal circumstances, the magnetization corresponds to that of bars of permanent magnetic material aligned as shown in Figure 4.

Figure 4:Ideal Magnetization of Track

Traditionally, the read head was the same type of a ring-shaped electromagnet with a gap, in practice the write head doubled as the read head. The changes in the magnetic fields on the track would induce a read current that reflects the changes in the magnetic flux. Figure 5 shows the idealized relation between the writing of a track and the subsequent reading of the track. The write current controls directly the orientation of the magnetic field emanating from the gap. Under ideal circumstances, the track magnetization switches orientation exactly under the head position when the write current switched. Since however the head is some distance of the track, and since thus the head magnitizes the media some distance away from the head, the switch in the current overwrites a small portion of the immediate preceeding magnetization. (This is dealt with in write precompensation, where the write current is switched slightly later to take this effect into account.) In addition, the magnetization of surrounding material affects the magnetization at any given point. As a result, the border between magnetization zones is in practice never straight but shows a wild zig-zag pattern. If the same head passes over the track, the flux changes emanating from the magnetization pattern on the track induce a current. Since the head picks up flux changes and ultimately magnetization changes from some distance, the induced current is not a single spike, but is somewhat spread out. Other than that, the read current is the derivative of the write current. By "peak detection" (e.g., electronic differnentiation and zero crossing detection), a magnetic read discovers the flux changes and ultimately the historic changes in the write current that encode the stored data.

Figure 5:Writing and Reading with a Gap Head. From top to bottom: write current, magnetization pattern, read current.

Perpendicular recording is done with a probe device (Figure 6). Perpendicular recording has no inherent advantages over longitudinal recording, but is being pursued in parallel by the magnetic recording industry because of the potential of better magnetization retention in some materials. Devices like MEMS are probe devices and would use perpendicular recording.

Figure 6:Perpendicular Recording with a Probe Head.

Nowadays, reading magnetic tracks is done using the magneto-resistive effect (Figure 7). The resistance of certain materials changes noticeably if a magnetic field is applied to them. The magnetic field alters the direction of a current slightly. The resistance of the magneto-resistive compound increases noticeably if the current direction is not aligned with the cristalline structure. This effect can be used to directly measure the magnetic flux, and hence the magnetization patterns on the track.

Figure 7:Magneto-Resistive Effect: The magnetic field (red) moves the electron flow in the sense current (yellow) up by an angle θ. The magneto-resistive material is in blue, the current conducts in brown.