Abstract

This mini-review deals with P-plant nutrition starting from the crude P-source, its further processing, most recent alternative P-sources, and biotechnological solutions of existing problems. Special attention is given to microbial P solubilization in fermentation systems as an alternative of chemical P-fertilizer production. Another emphasis of the mini-review is on the biofertilizer production and formulation.

Highlights

  • P is quite abundant in many soils, it is added to soil-plant systems in the form of phosphate fertilizers

  • Phosphorus (P) is one of the major nutrients limiting plant growth

  • During the last 10-15 years, scientists working in this field focused their studies in two main directions: A) Changing the traditional rock phosphate chemical dissolution scheme and finding alternative sources of P; B) Preparation of formulated biofertilizers with P-solubilizing activity

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Summary

Introduction

P is quite abundant in many soils, it is added to soil-plant systems in the form of phosphate fertilizers. Traditional P fertilizer production is based on chemical processing of insoluble mineral high-grade rock phosphate-what is calcium phosphate combined with quartz, calcite, dolomite, clay, iron oxide, carbonates, and alkali compounds. During the last 10-15 years, scientists working in this field focused their studies in two main directions: A) Changing the traditional rock phosphate chemical dissolution scheme and finding alternative sources of P; B) Preparation of formulated biofertilizers with P-solubilizing activity.

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