z-logo
Premium
Tillage and fertilizing effects on sandy soils. Review and selected results of long‐term experiments at Humboldt‐University Berlin
Author(s) -
Ellmer Frank,
Peschke Heinz,
Köhn Wolfgang,
Chmielewski FrankM.,
Baumecker Michael
Publication year - 2000
Publication title -
journal of plant nutrition and soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 1436-8730
DOI - 10.1002/1522-2624(200006)163:3<267::aid-jpln267>3.0.co;2-z
Subject(s) - plough , tillage , agronomy , phosphorus , soil water , organic matter , manure , soil organic matter , environmental science , irrigation , soil carbon , humus , chemistry , soil science , biology , organic chemistry
The Humboldt‐University of Berlin conducts several long‐term field trials designed to assess the effects of tillage methods, crop rotations, organic fertilization, mineral nitrogen, phosphorus, and potassium fertilizers, liming, irrigation, and weather conditions. On silty sand soils shallow ploughing resulted in a distinct accumulation of soil organic matter and phosphorus in the tilled soil layer while potassium and pH values were unaffected. On average shallow ploughing increased yields, with a tendency for higher yields in spring crops and lower yields in winter cereals. Different amounts of organic and mineral fertilizers applied over 30 years resulted in a great differentiation in soil organic matter content. In the following 32 years this variation stayed more or less unchanged, but with an overall reduction in the carbon content. In variants in which phosphate and potassic fertilizers were omitted, 16 kg ha —1 P and 15 kg ha —1 K per year were still being mobilized in the soil after 60 years. In treatments with mineral fertilization, the phosphorus is nearly balanced whilst only 60 % of the potassium is withdrawn from the soil. Additional organic fertilizers, given as farm yard manure, led to a nutrient surplus of 19 kg ha —1 a —1 P and 99 kg ha —1 a —1 K. Omitted liming caused an acidification of the soil to such an extent that crop production became impossible.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here