Siemens volt to Franklin second

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.

Franklin (1706–1790) was the American polymath who proved lightning is electrical with his famous kite experiment in 1752. He introduced the convention of "positive" and "negative" charge that we still use today. He arbitrarily assigned positive to the charge on glass rubbed with silk — which turned out to be a deficit of electrons, giving us the unfortunate convention that current flows opposite to electron motion.

The roentgen (R) was defined in 1928 as the radiation exposure producing 1 ESU of charge (1 franklin ≈ 3.336 × 10⁻¹⁰ C) per cm³ of dry air at STP. This CGS-era definition stuck because radiation safety regulations were already built around it. Even though the SI gray replaced the roentgen for dosimetry, the roentgen — and its franklin-based definition — persists in US regulatory and medical imaging contexts.

The legacy unit of radiation exposure, the roentgen (R), is defined as the amount of X-ray or gamma radiation that produces 1 esu of charge (1 franklin) per cubic centimeter of dry air at STP. This definition dates from the 1920s when CGS-ESU was standard. Modern dosimetry uses grays and sieverts, but the roentgen and its franklin-based definition persist in some medical and regulatory contexts.

One Fr/s is about 0.33 nanoamperes — less current than a sleeping microcontroller draws. To equal the 1 A flowing through a phone charger cable, you would need about 3 billion franklins per second. The unit is spectacularly impractical for anything beyond electrostatics calculations.

Sort of. He labelled the charge on glass rubbed with silk as "positive," not knowing it was caused by removing electrons. When Thomson discovered the electron in 1897, it turned out electrons carry what Franklin called negative charge. So conventional current flows from + to −, opposite to actual electron flow. Engineers and physicists have lived with this "mistake" for over 250 years.