Copyright © Philip M. Parker, INSEAD. Terms of Use.
| Domain | Definition |
Geological | This destructive analytical technique is used to determine concentrations of specific chemical elements based on their rates of molecular diffusion in a gaseous or vaporous mixture. A known quantity of the chemical element in question is added to the mixture. This quantity, referred to as a tracer, is monitored to measure its diffusion rate. (references) |
Source: compiled by the editor from various references; see credits. | |
Hexadecimal (or equivalents, 770AD-1900s) (references)49 53 4F 54 4F 50 45 2D 44 49 4C 55 54 49 4F 4E 4D 41 53 53 53 50 45 43 54 52 4F 4D 45 54 52 59 |
| Leonardo da Vinci (1452-1519; backwards) (references)
|
Binary Code (1918-1938, probably earlier) (references)01001001 01010011 01001111 01010100 01001111 01010000 01000101 00101101 01000100 01001001 01001100 01010101 01010100 01001001 01001111 01001110 00100000 01001101 01000001 01010011 01010011 00100000 01010011 01010000 01000101 01000011 01010100 01010010 01001111 01001101 01000101 01010100 01010010 01011001 |
HTML Code (1990) (references)I S O T O P E - D I L U T I O N   M A S S   S P E C T R O M E T R Y |
ISO 10646 (1991-1993) (references)0049 0053 004F 0054 004F 0050 0045 002D 0044 0049 004C 0055 0054 0049 004F 004E 004D 0041 0053 0053 0053 0050 0045 0043 0054 0052 004F 004D 0045 0054 0052 0059 |
Encryption (beginner's substitution cypher): (references)435349544950391538434655544349482473553532535039375452494739545259 |
| 1. Orthography 2. Bibliography |
Copyright © Philip M. Parker, INSEAD. Terms of Use.
