Soil carbon and phosphorus pools in field crop rotations in pampean soils of Argentina
In temperate cropping systems, a better understanding of soil C and P transformations is pertinent to evaluate crop management consequences in the medium term. Six-year cropping systems experiments consisting of corn [Zea mays L.]-double-cropped wheat [Triticum aestivum L.]/soybean [Glycine max [L.]...
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| 100 | 1 | |a Ciampitti, Ignacio Antonio |9 46012 | |
| 245 | 1 | 0 | |a Soil carbon and phosphorus pools in field crop rotations in pampean soils of Argentina |
| 520 | |a In temperate cropping systems, a better understanding of soil C and P transformations is pertinent to evaluate crop management consequences in the medium term. Six-year cropping systems experiments consisting of corn [Zea mays L.]-double-cropped wheat [Triticum aestivum L.]/soybean [Glycine max [L.] Merr.] [two sites] and corn-soybean-double-cropped wheat/soybean [two sites], with [Fp] or without P added [Wp], were evaluated in the Pampean soils of Argentina. The objectives were [i] to quantify the effects of continuous P fertilization on the size and vertical distribution of C and P in total organic C [TOC] and particulate organic matter [POM] fractions and [ii] to evaluate the POM-P fraction as a potential indicator of crop P availability. Annually, an average P rate of 34 kg P ha -1 was applied in Fp plots. The TOC, total P [TP], POM-C, and POM-P were measured in the 0- to 5-, 5- to 10-, and 10- to 20-cm soil depths at the end of the 6-yr period. Phosphorus fertilization increased TOC from 0.5 to 2.5 g C kg -1 and TP from 24.1 to 77.4 mg P kg -1 in the 0- to 20-cm depth. The POM-C and POM-P fractions were more sensitive than TOC or TP to P fertilization, increasing by 14 and 47 percent, respectively, in the 0- to 20-cm depth under continuous P addition. The greatest diff erences in POM-C and POM-P among treatments occurred in the surface soil layer. A signifi cant relationship was found between POM-P and corn P uptake at anthesis. | ||
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| 700 | 1 | |9 6390 |a Rubio, Gerardo | |
| 773 | |t Soil Science Society of America Journal |g Vol.75, no.2 (2011), p.616-625 | ||
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| 900 | |a ^tSoil carbon and phosphorus pools in field crop rotations in pampean soils of Argentina | ||
| 900 | |a ^aCiampitti^bI.A. | ||
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| 900 | |a ^aCiampitti^bI.A.^tIPNI Latin American Southern Cone, Av. Santa Fe 910, B1641ABO, Acassuso, Buenos Aires, Argentina | ||
| 900 | |a ^aGarcÃa^bF.O.^tAgronomy Dep., Purdue Univ., 915 West State Street, West Lafayette, IN 47907-2054, United States | ||
| 900 | |a ^aPicone^bL.I.^tFCA-INTA Balcarce, National Univ. of Mar Del Plata, CC 276, 7620 Balcarce, Buenos Aires, Argentina | ||
| 900 | |a ^aRubio^bG.^tAgricultural College, INBA, Univ. of Buenos Aires, Av. San Martin 4453, C1417DSE Buenos Aires, Argentina | ||
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| 900 | |a SOIL CARBON | ||
| 900 | |a SOIL DEPTH | ||
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| 900 | |a TOTAL ORGANIC C | ||
| 900 | |a VERTICAL DISTRIBUTIONS | ||
| 900 | |a WHEAT [TRITICUM AESTIVUM L.] | ||
| 900 | |a AMINO ACIDS | ||
| 900 | |a CROPS | ||
| 900 | |a NITROGEN FIXATION | ||
| 900 | |a PHOSPHORUS | ||
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| 900 | |a CROP ROTATION | ||
| 900 | |a EXPERIMENTAL STUDY | ||
| 900 | |a FERTILIZER APPLICATION | ||
| 900 | |a MAIZE | ||
| 900 | |a NUTRIENT AVAILABILITY | ||
| 900 | |a NUTRIENT UPTAKE | ||
| 900 | |a PARTICULATE ORGANIC MATTER | ||
| 900 | |a SIZE DISTRIBUTION | ||
| 900 | |a SOIL CARBON | ||
| 900 | |a SOYBEAN | ||
| 900 | |a TOTAL ORGANIC CARBON | ||
| 900 | |a TRANSFORMATION | ||
| 900 | |a VERTICAL DISTRIBUTION | ||
| 900 | |a WHEAT | ||
| 900 | |a ARGENTINA | ||
| 900 | |a PAMPAS | ||
| 900 | |a In temperate cropping systems, a better understanding of soil C and P transformations is pertinent to evaluate crop management consequences in the medium term. Six-year cropping systems experiments consisting of corn [Zea mays L.]-double-cropped wheat [Triticum aestivum L.]/soybean [Glycine max [L.] Merr.] [two sites] and corn-soybean-double-cropped wheat/soybean [two sites], with [Fp] or without P added [Wp], were evaluated in the Pampean soils of Argentina. The objectives were [i] to quantify the effects of continuous P fertilization on the size and vertical distribution of C and P in total organic C [TOC] and particulate organic matter [POM] fractions and [ii] to evaluate the POM-P fraction as a potential indicator of crop P availability. Annually, an average P rate of 34 kg P ha -1 was applied in Fp plots. The TOC, total P [TP], POM-C, and POM-P were measured in the 0- to 5-, 5- to 10-, and 10- to 20-cm soil depths at the end of the 6-yr period. Phosphorus fertilization increased TOC from 0.5 to 2.5 g C kg -1 and TP from 24.1 to 77.4 mg P kg -1 in the 0- to 20-cm depth. The POM-C and POM-P fractions were more sensitive than TOC or TP to P fertilization, increasing by 14 and 47 percent, respectively, in the 0- to 20-cm depth under continuous P addition. The greatest diff erences in POM-C and POM-P among treatments occurred in the surface soil layer. A signifi cant relationship was found between POM-P and corn P uptake at anthesis. | ||
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