Where the ground comes from
Five ways a surface ends up exposed and loaded.
They look alike from a monitor and carry different chemistry, so sampling comes before 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, and still wet enough to be chemically busy.
Brine and evaporation ponds. Desalination is a Gulf-scale industry: one 2019 estimate put global brine production at about 142 million cubic meters a day, with Saudi Arabia, the UAE, Kuwait and Qatar responsible for 55 percent of it. Evaporation ponds that take it leave crust behind with whatever arrived in the feed.
Tailings, spoil and disturbed ground. Mining, quarrying, construction and demolition surfaces, where the operation produced the material and somebody usually already holds an analysis of it.
Abandoned irrigated land. FAO puts salt-affected soils at 1,381 million hectares, roughly a tenth of the world's cropland among them. Ground salinized out of production dries and crusts with a farming history in the profile.
Oil-affected shore and beach. A spill loads a shoreline in hours. Responders recover what can be lifted, and the hydrocarbon chemistry bound into sand, shingle and marsh sediment stays where it is, which is the fraction an oxidation assist works.
What is in the ground varies more between the five than the ground itself does, and so do the budget, the measurement problem and the person who has to sign.