Macronutrients — nitrogen, phosphorus, potassium, calcium, magnesium, sulfur — are the structural and energetic raw materials plants consume in measurable percentages of dry matter. Trace minerals are the cofactors. Iron, manganese, zinc, copper, boron, molybdenum, nickel, and dozens of ultra-trace elements each catalyze specific enzymatic reactions — chlorophyll synthesis, nitrogen fixation, hormone regulation, lignin formation, sugar transport. Without them, the macronutrient pool is biochemically inert.
The Azomite ore is hydrated sodium calcium aluminosilicate (HSCAS) — a complex silica matrix that holds its trace mineral inventory in a slow-release form. The fraction that is plant-available depends on soil pH, microbial activity, root exudates, and time. This is why Azomite is positioned as a soil-building amendment rather than a fast-correction product: in mineral-depleted soils, regular application over multiple seasons rebuilds the trace mineral pool the soil food web draws from.
The independent research literature is concentrated on tomato and pepper. Peer-reviewed greenhouse work at UC Berkeley / USDA-ARS reported statistically significant increases in fruit number per plant when Azomite was applied at 5% by weight in soil or 4.5 g per plant per month via drip (Mehlferber et al. 2022, Applied & Environmental Microbiology). A Colorado State University field trial on certified-organic pepper reported a 68% increase in red-fruit weight per plant at 100 lb/acre banded in-row, with response varying by cultivar (Uchanski & Mason, CSU Extension, 2017). For broadacre crops the published evidence base is narrower — the field rates published in this product page are manufacturer recommendations that fall within the range validated in the CSU work.
For a deeper read on the broader category, see The 5 Fertilizers That Will Also Encourage Soil Health and How Do Soil Microbes Affect Plant Health.