Many physical, chemical, and mineralogical factors govern the release of K from micas by cation exchange reaction and dissolution processes. Mainly in Indian agricultural conditions, most of the farmers use only nitrogen and phosphorus and do not use the potassic fertilizer due to unawareness that the problem of K deficiency occurs in soils and it is reported that~72 % of soils need immediate K fertilization for good crop production. The efficient soil microorganisms influence the availability of minerals in soil and play a major role in ion cycling and soil fertility. A number of microorganisms such as bacteria (Bacillus mucilaginosus, B. edaphicus, B. circulans, B. cereus, B. subtilis, B. coagulans, B. amyloliquefaciens, B. megaterium, Enterobacter hormaechei, Flectobacillus spp., Acidithiobacillus ferrooxidans, Paenibacillus spp.), fungal strains (Aspergillus niger, A. fumigatus, and A. terreus), and yeast (Torulaspora globosa) solubilize the insoluble K to soluble forms of K for plant uptake. The main mechanisms of KSMs are acidolysis, chelation, exchange reactions, complexolysis, and production of organic acids. Therefore, the efficient KSMs should be applied for solubilization of unavailable form of K to an available form of K that is taken up by the plant for their growth and development. Therefore, our aim is to elaborate on the studies of native K-solubilizing microbes to develop efficient microbial consortium and their uses as biofertilizers or a biocontrol agent, which helps to enhance the K availability in agricultural soils and increase crop production and environmental and agricultural sustainability.