NEEDS FOR CONTROLLED-AVAILABILITY MICRONUTRIENT FERTILIZERS

Authors
Citation
Jj. Mortvedt, NEEDS FOR CONTROLLED-AVAILABILITY MICRONUTRIENT FERTILIZERS, Fertilizer research, 38(3), 1994, pp. 213-221
Citations number
NO
Categorie Soggetti
Agriculture Soil Science
Journal title
ISSN journal
01671731
Volume
38
Issue
3
Year of publication
1994
Pages
213 - 221
Database
ISI
SICI code
0167-1731(1994)38:3<213:NFCMF>2.0.ZU;2-L
Abstract
Use of micronutrients for agronomic and horticultural crops has increa sed markedly in recent years. Increased use is related to higher nutri ent demands from more intensive cropping practices and also from farmi ng marginal lands. Most of the fertilizers used to correct micronutrie nt deficiencies are water- soluble inorganic sources or soluble organi c products such as synthetic chelates or natural organic complexes. Th ese fertilizers may react with soil to decrease their availability to plants. The rates of such chemical reactions may differ considerably w ith each micronutrient fertilizer and soil environment. Recommended mi cronutrient rates have been based on results of numerous experiments, and these rates vary with crop, soil, and other factors. The usual app lication rates (on an elemental basis) range from 1 to 10 kg ha-1 for Cu, Fe, Mn and Zn; < 1 kg ha-1 for B; and < 100 g ha-1 for Mo. Because the metallic micronutrients (Cu, Fe, Mn, and Zn) generally are sorbed strongly by soil clays, they do not move significantly in soil. Hence , they are not leached readily from the zone of application to lower s oil depths or into groundwaters. Mobility of these micronutrient catio ns is higher in sandy soils, especially with high leaching conditions. Therefore, their movement out of the root zone is possible under some situations. Significant residual effects of soluble Cu and Zn sources greatly reduce the need for controlled-availability Cu and Zn product s. Controlled-availability Fe and Mn fertilizers have not been effecti ve because the rapid oxidation of Fe and Mn and reactions with soil re duce their availability upon release. Because soluble B fertilizers fo rm boric acid molecules in soil, they are mobile and subjects to leach ing conditions. While mobility of B is less than that of NO3(-)-N in s oil, field results have demonstrated loss of applied B from the root z one in sandy soils. Slightly soluble B fertilizers, such as colemanite and ulexite, and fritted B products (powdered glass-like materials wh ose solubility is controlled by particle size) have been used in sandy soils for some crops. Molybdenum requirements are much lower than tho se of the other micronutrients. Deficiencies generally are corrected b y liming the soil or by seed or foliar applications, so there is littl e need for controlled-availability Mo fertilizers. Little research has been conducted on controlled availability micronutrient fertilizers. While fritted products are considered in this category, they are diffi cult to handle and only may be of value in supplying B under specific conditions. Coating soluble granular micronutrient fertilizers also ha s been attempted, but there are few reported results of their relative effectiveness in comparison with conventional fertilizers and applica tion methods. New micronutrient products may be needed for specific co nditions such as greenhouse-culture or container-grown crops, but plan t needs also may be met by multiple applications of soluble sources.