Mineralnivåene

Mineralnivåene, literally “the mineral levels,” refer to the quantitative measurements of mineral content within a given medium. The term is employed across several scientific disciplines, including geology, agronomy, environmental science, and medical diagnostics. In a geological context, mineralnivåene describe the abundance of specific minerals in rock strata, soil profiles, or sedimentary layers. Geologists rely on these values to reconstruct depositional environments, assess mineral resources, and evaluate geological processes such as weathering and diagenesis. Typical analysis uses X‑ray fluorescence, inductively coupled plasma mass spectrometry (ICP‑MS), or optical mineralogy.

In agriculture, mineralnivåene represent the nutrient concentrations available in soil, water, and plant tissues. Soil tests that quantify macro‑minerals—nitrogen, phosphorus, potassium—and micro‑minerals—zinc, copper, iron—guide fertilisation management and are critical for maintaining crop productivity and preventing environmental contamination. These measurements are standardized through national and international protocols (e.g., ISO 10683 for peat analysis).

Within human health, mineralnivåene are the levels of essential trace elements and macrominerals in blood, urine, or hair. Clinical laboratories measure serum calcium, magnesium, iron, and zinc to diagnose deficiencies or toxicities. Standard reference ranges depend on age, sex, and laboratory calibration, and are crucial for monitoring conditions such as osteoporosis, anemia, and metabolic disorders.

Industrial applications of mineralnivåene include quality control in mining, metallurgy, and construction materials. By quantifying ore grade, slag composition, or aggregate mineralogy, engineers can optimise extraction processes, ensure product specifications, and assess environmental impact.

Across all contexts, accurate determination of mineralnivåene supports decision‑making, resource management, and scientific understanding.