Complementary irrigation and direct drilling have little effect on soil organic carbon content in semiarid Argentina

Irrigation and tillage modify soil properties. The aim of the present study was to evaluate the simultaneous effect of complementary irrigation and zero tillage [ZT] on soil organic carbon [SOC]. Two treatments [irrigated and rain fed soils] were evaluated in a field experiment set up in Manfredi, C...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autor principal: Giubergia, Juan Pablo
Otros Autores: Martellotto, Eduardo Enrique, Lavado, Raúl Silvio
Formato: Artículo
Lenguaje:Inglés
Materias:
Acceso en línea:http://ri.agro.uba.ar/files/intranet/articulo/2013giubergia.pdf
LINK AL EDITOR
Aporte de:Registro referencial: Solicitar el recurso aquí
LEADER 06945cab a22014297a 4500
001 AR-BaUFA000457
003 AR-BaUFA
005 20211221122922.0
008 181208t2013 |||||o|||||00||||eng d
999 |c 46891  |d 46891 
022 |a 0167-1987 
024 |a 10.1016/j.still.2013.08.003 
040 |a AR-BaUFA  |c AR-BaUFA 
100 1 |9 31270  |a Giubergia, Juan Pablo 
245 0 0 |a Complementary irrigation and direct drilling have little effect on soil organic carbon content in semiarid Argentina 
520 |a Irrigation and tillage modify soil properties. The aim of the present study was to evaluate the simultaneous effect of complementary irrigation and zero tillage [ZT] on soil organic carbon [SOC]. Two treatments [irrigated and rain fed soils] were evaluated in a field experiment set up in Manfredi, Córdoba province, Argentina. The soil was grid-sampled at the beginning of the experiment in 1996 and soil organic carbon [SOC], aggregate stability [AS], bulk density [BD], electrical conductivity [EC] and exchangeable sodium percentage [ESP] were determined in 2007. In the irrigated treatment SOC tended to increase on the surface layer in the irrigated experiment. The increase in SOC stock was estimated as 0.221tnC/ha/year but higher C-CO2 emission also occurred. The AS of the surface horizon was higher under irrigation, associated with SOC and soil EC. The quasi-equilibrium in SOC was explained by a greater intake of crop residues counteracted by an increased biological activity in the irrigated soil. 
653 0 |a COMPLEMENTARY IRRIGATION 
653 0 |a SOIL ORGANIC CARBON 
653 0 |a STRUCTURAL STABILITY 
653 0 |a AGGREGATE STABILITY 
653 0 |a ELECTRICAL CONDUCTIVITY 
653 0 |a EXCHANGEABLE SODIUM PERCENTAGES 
653 0 |a QUASI-EQUILIBRIUM 
653 0 |a SIMULTANEOUS EFFECTS 
653 0 |a STRUCTURAL STABILITIES 
653 0 |a AGRICULTURAL WASTES 
653 0 |a BIOACTIVITY 
653 0 |a CARBON DIOXIDE 
653 0 |a EXPERIMENTS 
653 0 |a SOIL MOISTURE 
653 0 |a STABILITY 
653 0 |a IRRIGATION 
653 0 |a BULK DENSITY 
653 0 |a DRILLING 
653 0 |a ELECTRICAL CONDUCTIVITY 
653 0 |a RAINFED AGRICULTURE 
653 0 |a SEMIARID REGION 
653 0 |a SOIL ORGANIC MATTER 
653 0 |a SOIL PROPERTY 
653 0 |a TILLAGE 
653 0 |a ZERO TILLAGE 
653 0 |a ARGENTINA 
653 0 |a CORDOBA [ARGENTINA] 
700 1 |9 33902  |a Martellotto, Eduardo Enrique 
700 1 |9 24365  |a Lavado, Raúl Silvio 
773 |t Soil and Tillage Research  |g vol.134 (2013), p.147-152 
856 |u http://ri.agro.uba.ar/files/intranet/articulo/2013giubergia.pdf  |i En reservorio  |q application/pdf  |f 2013giubergia  |x MIGRADOS2018 
856 |u http://www.elsevier.com/  |x MIGRADOS2018  |z LINK AL EDITOR 
900 |a as 
900 |a 20141009 
900 |a N13 
900 |a SCOPUS 
900 |a N13SCOPUS 
900 |a a 
900 |a s 
900 |a ARTICULO 
900 |a EN LINEA 
900 |a 01671987 
900 |a 10.1016/j.still.2013.08.003 
900 |a ^tComplementary irrigation and direct drilling have little effect on soil organic carbon content in semiarid Argentina 
900 |a ^aGiubergia^bJ.P. 
900 |a ^aMartellotto^bE. 
900 |a ^aLavado^bR.S. 
900 |a ^aGiubergia^bJ. P. 
900 |a ^aMartellotto^bE. E. 
900 |a ^aLavado^bR. S. 
900 |a   
900 |a ^aGiubergia^bJ.P.^tNational Institute for Agricultural Technology [INTA], Manfredi Experimental Station, Ruta 9 km 636, 5988 Manfredi, Córdoba, Argentina 
900 |a ^aMartellotto^bE.^tResearch Institute for Biosciences in Agronomy and Environment [INBA], Facultad de Agronomía, Avda. San Martín 4453, Buenos Aires 1417, Argentina 
900 |a ^aLavado^bR.S. 
900 |a ^aGiubergia, J.P^tNational Institute for Agricultural Technology (INTA), Manfredi Experimental Station, Ruta 9 km 636, 5988 Manfredi, Córdoba, Argentina 
900 |a ^aMartellotto, E^tNational Institute for Agricultural Technology (INTA), Manfredi Experimental Station, Ruta 9 km 636, 5988 Manfredi, Córdoba, Argentina 
900 |a ^aLavado, R.S^tResearch Institute for Biosciences in Agronomy and Environment (INBA), Facultad de Agronomía, Avda^tSan Martín 4453, Buenos Aires 1417, Argentina 
900 |a ^tSoil and Tillage Research^cSoil Tillage Res. 
900 |a en 
900 |a 147 
900 |a ^i 
900 |a Vol. 134 
900 |a 152 
900 |a COMPLEMENTARY IRRIGATION 
900 |a SOIL ORGANIC CARBON 
900 |a STRUCTURAL STABILITY 
900 |a AGGREGATE STABILITY 
900 |a ELECTRICAL CONDUCTIVITY 
900 |a EXCHANGEABLE SODIUM PERCENTAGES 
900 |a QUASI-EQUILIBRIUM 
900 |a SIMULTANEOUS EFFECTS 
900 |a STRUCTURAL STABILITIES 
900 |a AGRICULTURAL WASTES 
900 |a BIOACTIVITY 
900 |a CARBON DIOXIDE 
900 |a EXPERIMENTS 
900 |a SOIL MOISTURE 
900 |a STABILITY 
900 |a IRRIGATION 
900 |a BULK DENSITY 
900 |a DRILLING 
900 |a ELECTRICAL CONDUCTIVITY 
900 |a RAINFED AGRICULTURE 
900 |a SEMIARID REGION 
900 |a SOIL ORGANIC MATTER 
900 |a SOIL PROPERTY 
900 |a TILLAGE 
900 |a ZERO TILLAGE 
900 |a ARGENTINA 
900 |a CORDOBA [ARGENTINA] 
900 |a Irrigation and tillage modify soil properties. The aim of the present study was to evaluate the simultaneous effect of complementary irrigation and zero tillage [ZT] on soil organic carbon [SOC]. Two treatments [irrigated and rain fed soils] were evaluated in a field experiment set up in Manfredi, Córdoba province, Argentina. The soil was grid-sampled at the beginning of the experiment in 1996 and soil organic carbon [SOC], aggregate stability [AS], bulk density [BD], electrical conductivity [EC] and exchangeable sodium percentage [ESP] were determined in 2007. In the irrigated treatment SOC tended to increase on the surface layer in the irrigated experiment. The increase in SOC stock was estimated as 0.221tnC/ha/year but higher C-CO2 emission also occurred. The AS of the surface horizon was higher under irrigation, associated with SOC and soil EC. The quasi-equilibrium in SOC was explained by a greater intake of crop residues counteracted by an increased biological activity in the irrigated soil. 
900 |a 134 
900 |a 2013 
900 |a ^cH 
900 |a AAG 
900 |a AGROVOC 
900 |a 2013giubergia 
900 |a AAG 
900 |a http://ri.agro.uba.ar/files/intranet/articulo/2013giubergia.pdf 
900 |a 2013giubergia.pdf 
900 |a http://www.elsevier.com/ 
900 |a http://www.scopus.com/inward/record.url?eid=2-s2.0-84883540759&partnerID=40&md5=7608f5a8c61fb47b89c26d8553d1bdee 
900 |a ^a^b^c^d^e^f^g^h^i 
900 |a OS 
942 0 0 |c ARTICULO  |2 udc 
942 0 0 |c ENLINEA  |2 udc