Why does carbon increase in highly weathered soil under no-till upon lime and gypsum use?

Science of the Total Environment

Volumn 599-600, Issue , 2017, Pages 523-532

  Inagaki, Thiago Massao ^a   de Moraes Sá, João Carlos ^b   Caires, Eduardo Fávero ^b   Gonçalves, Daniel Ruiz Potma ^b  

^a TECHNICAL UNIVERSITY OF MUNICH   (Germany)

^b STATE UNIVERSITY OF PONTA GROSSA   (Brazil)

Author keywords

Acid soils; Carbon sequestration; Incubation; Soil biology; Soil correction; Soil organic matter

Indexed keywords

AGRICULTURAL WASTES; AGRICULTURE; CALCIUM; GYPSUM; LIME; ORGANIC CARBON; SOIL CONDITIONERS; SOIL CONSERVATION; SOIL SURVEYS;

ACID SOILS; CARBON SEQUESTRATION; INCUBATION; SOIL BIOLOGY; SOIL ORGANIC MATTERS;

SOILS;

CALCIUM ION; CALCIUM OXIDE; CALCIUM SULFATE; CARBON; ORGANIC CARBON; SOIL ORGANIC MATTER;

ACID SOIL; CARBON SEQUESTRATION; GYPSUM; LIME; MICROBIAL ACTIVITY; ORGANIC CARBON; SOIL MICROORGANISM; SOIL ORGANIC MATTER;

ARTICLE; BRAZIL; COMPLEX FORMATION; CONSERVATION TILLAGE; CONTROLLED STUDY; CORRELATIONAL STUDY; CROP PRODUCTION; FIELD EXPERIMENT; INCUBATION TIME; MICROBIAL ACTIVITY; NO TILLAGE; PLANT RESIDUE; SIMULATION; SOIL AMENDMENT; SOIL FERTILITY; SOIL PROPERTY; SURFACE AREA; WEATHERING;

BRAZIL;

EID: 85018727938     PISSN: 00489697     EISSN: 18791026     Source Type: Journal    
DOI: 10.1016/j.scitotenv.2017.04.234     Document Type: Article

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