https://www.selleckchem.com/products/fl118.html
If N input remains constant as noted in 2020 (S3) or decreases by 1% annually (S4), a reduction of up to 52%-67% in carbonates dissolution is expected compared to the BAU. The presence of CaCO3 in the soil is important for various processes including acidity buffering, aggregates formation and stabilization, organic matter stabilization, microbial and enzyme activities, nutrients cycling and availability, and water permeability and plants productivity. Therefore, optimizing N fertilization and improving N use efficiency are important for
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