Open AccessInfluence of Conservative and Conventional Soil Technologies on Physical, Chemical and Biolocical Properties of an Argic Chernozem Belong to Caracal Area
Author(s) -
Venera Mihaela Stroe,
Irina Calciu,
Monica Stanciu Burileanu,
Lavinia Pârvan
Publication year - 2011
Publication title -
bulletin of university of agricultural sciences and veterinary medicine cluj-napoca. agriculture
Language(s) - English
Resource type - Journals
eISSN - 1843-5386
pISSN - 1843-5246
DOI - 10.15835/buasvmcn-agr:6465
Subject(s) - chernozem , tillage , environmental science , soil fertility , aeration , soil retrogression and degradation , soil structure , soil science , soil biodiversity , agriculture , agronomy , soil water , ecology , biology
Continuous use of traditional tillage system (conventional) resulted in a gradual harvest increase, but gave rise to some worrying negative phenomenon regarding the most important supply of the agricultural production - soil, by its chemical and physical degradation.This paper aims to assess soil degradation processes, based on pedo-transfer rules and is based on of expeditionary studies regarding assessment and characterization of soil fertility, under the practice of various farming systems: conventional tillage and minimum tillage.
The study carried out the effects of moderat conservative tillage on physical and chemical soil properties comparative with conventional soil technology on an argic chernozem, belongs to the agricultural Caracal area. Agricultural area is affected by a relatively high variability of the limiting factors and soil degradation processes, which require adaptation of technology systems to protection of soil and plants. Because of all limiting factors, natural and antropic, in this expeditionary study we compare the moderat conservative tillage effects, with conventional technology effects and impact of those both soil technology, on physical, chemical and biological properties.
Results of study show the potential depth of aeration conditions are moderately favorable, being determined particularly by intense state of compactness of the soil as a natural consequence of it.
Macroporosity decrease in depth, has negative consequences not only on the normal performance of the processes of aeration, and water penetration and infiltration, but for the accumulation of water available for plants. Content of structural microagregates water-stable or soil dispersion is high, which shows that the formation of structural macroagregates occurred more mechanical factors such as compaction or natural processes. The numerical values of the degree of compaction of 15-20 cm in depth up to the 15-18% v / v in both phases of observation. Deep compaction is undoubtedly due to the technological system applied to the greatest extent, and only a small part pedogenetical natural factors.