Siemens volt to CGS e.m. unit

In nodal admittance matrix analysis of power grids and RF networks, bus currents are computed as the product of an admittance matrix (siemens) and a voltage vector (volts). The intermediate result is naturally in S·V before being labelled as amperes. It is a computational stepping stone rather than a measurement unit.

The siemens (S) is the SI unit of electrical conductance — the reciprocal of resistance in ohms. One siemens means one ampere flows per volt applied. It is named after Werner von Siemens (1816–1892), German inventor and industrialist who founded the Siemens company and pioneered telegraph and electrical engineering.

In complex networks with many parallel paths, adding conductances (siemens) is simpler than combining resistances — parallel conductances just add, like parallel resistances require reciprocal math. Power system load-flow software uses admittance (Y = G + jB in siemens) matrices because they are sparse and computationally efficient.

Yes, dimensionally they are both equal to one ampere: S·V = (A/V)·V = A, and W/V = (V·A)/V = A. The difference is conceptual — S·V emphasizes conductance times voltage (Ohm's law), while W/V emphasizes power divided by voltage (the power equation). Same number, different story.

Power grids have thousands of buses and transmission lines. The admittance matrix is large but very sparse (most buses connect to only a few neighbors), making it ideal for efficient numerical solvers. Expressing branch currents as Y·V (siemens times volts) enables Newton-Raphson load flow algorithms that converge in just 3–5 iterations for most grids.

The CGS e.m. unit of current (10 A) was inconveniently large for everyday lab work, while the CGS e.m. unit of resistance (the abohm, 10⁻⁹ Ω) was absurdly small. Physicists created "practical" units — the ampere, volt, and ohm — as decimal multiples that gave human-scale numbers. The ampere was set at 0.1 abampere. These practical units eventually became SI, while the "absolute" CGS units became historical footnotes.

In the 19th century, electricity and magnetism were treated as partially separate phenomena, leading to separate "natural" unit choices. The EMU system normalized magnetic permeability to 1; the ESU system normalized electric permittivity to 1; the Gaussian system mixed both. Once Maxwell unified electromagnetism, this fragmentation became unnecessary — but the systems persisted in literature for a century.

They introduced "practical" units — the ampere, volt, and ohm — as decimal multiples of CGS-EMU quantities. The ampere was defined as 0.1 abampere (CGS e.m. unit). This practical system eventually became SI, while the "absolute" CGS units faded. The factor of 10 was chosen for human-scale convenience.

The gauss (magnetic flux density, = 10⁻⁴ tesla) remains surprisingly common — refrigerator magnets are rated in gauss, and MRI field strengths are often quoted in both tesla and gauss. The oersted (magnetic field strength) appears in materials science. These CGS-EMU holdouts persist because their numerical values are more convenient for everyday magnets.

The SI was officially adopted in 1960, but the transition took decades. Most physics journals required SI by the 1970s, though astrophysics and plasma physics held onto Gaussian CGS into the 2000s. Some subfields never fully switched — you can still find new papers using gauss and oersted alongside tesla and A/m.