Where the ground comes from
Four ways a surface starts emitting.
They look alike from a monitor and they behave differently under treatment, which is why the assessment comes before the equipment.
Receding water bodies. A lake, reservoir or inland sea losing area exposes sediment that has never met wind. Owens, the Aral, the Salton Sea. The freshly exposed margin is usually the most emissive part.
Brine and evaporation ponds. Desalination is a Gulf-scale industry: one 2019 estimate put global brine production at about 142 million cubic metres a day, with Saudi Arabia, the UAE, Kuwait and Qatar responsible for 55 per cent of it, though that figure reaches us through secondary coverage and is treated here as indicative. Where that brine goes into evaporation ponds, the ponds do their job and leave crust.
Tailings, spoil and disturbed ground. Mining, quarrying, construction and demolition surfaces, where the emissive material is generated rather than uncovered.
Abandoned irrigated land. FAO puts salt-affected soils at 1,381 million hectares, roughly a tenth of the world's cropland among them. Ground salinised out of production dries, crusts and joins the same category.
Owning one of those four is not the same as owning the others. The measurement problem, the budget it comes out of and the person who has to sign are different every time.