planck 1: each sheet, 16 × 32 = 512 elements, −+−+ as a chessboard. every element holds one charge, +1 or −1, and every neighbour it touches is the opposite sign, so each sheet is 976 + to − bonds and nets to zero. planck 0: the gold core. every gold atom is the same: one loose outer electron (6s¹), one hand to hold. the 256 + tips of each sheet reach into the gold. bond lets each tip take one gold atom's electron: the tip's + is paid off, the gold atom becomes Au⁺. at full bond the core is +512 and each sheet −256. total charge stays 0, but it's now split into layers, like a capacitor.

wind: three things smack into the top sheet at the scaler energy (0.01 eV to start: gas-molecule speeds; 3 × 0.01 = 0.03 eV is about room temperature). the water ion (H₃O⁺, +1) is steered by the −+−+ surface onto a − square and cancels it. the neutron has no charge, so the layers don't touch it; it crosses into the gold, where gold-197 can swallow it and become gold-198, which decays in 2.7 days into mercury-198. the D₂ molecule is neutral and needs 4.56 eV to break, so at wind speed it just bounces. the sizes: 1 cm squares, so the 512-unit gold core is 512 g, 0.52 mm thick.

gravity: your 1.6.5 × 10⁻³⁵ is the Planck length, 1.616 × 10⁻³⁵ m, so plank is Planck. every molecule that lands adds one of those as its graviton weight; gold's is that with .79 on the exponent, 2.62 × 10⁻³⁶ an atom. real gravity, for scale: Earth's pull over the last centimetre is a ten-millionth of a wind neutron's energy (two millionths for the heavier water ion), and the gold core's own pull is 2.3 billion times weaker than Earth's. at these speeds the paths are straight lines; the ×10⁷ button draws the droop so you can see which way it goes. a real graviton has no mass at all, so 1 p can be your unit for it, not its weight. ground PEWTER.