Managing Global Resources for a Secure Future

2017 Annual Meeting | Oct. 22-25 | Tampa, FL

105743 C and N Pools in a Brazilian Oxisol According to Tillage Systems and N Sources.

Poster Number 707

See more from this Division: SSSA Division: Soil and Water Management and Conservation
See more from this Session: Soil and Water Management and Conservation General Poster III

Wednesday, October 25, 2017
Tampa Convention Center, East Exhibit Hall

Rodrigo S. Nicoloso1, Charles W. Rice2, Roberto A. Grave3, Camila R. Wuaden4, Morgana Dalla Costa5 and Adriana Pigosso5, (1)Department of Agronomy, Kansas State University, Manhattan, KS
(2)2701 Throckmorton Hall, Kansas State University, Manhattan, KS
(3)Instituto Federal Catarinense, Concordia, Brazil
(4)UDESC, Lages, Brazil
(5)FACC, Concordia, Brazil
Poster Presentation
  • Nicoloso_CNpools.pdf (565.6 kB)
  • Abstract:
    We assessed the effects of tillage and sources of N on soil C and N pools in an Oxisol from Southern Brazil. The experiment was established in 2012 using split-plots with maize (Zea mays L.) and black oat (Avena strigosa (Scherb) L.) double cropping system with four replications. The main plots (25x10m) had two soil tillage systems: conventional tillage (CT) and no-tillage (NT). The sub-plots (5x10m) had 140 kg total-N ha-1 applied for maize either as urea (UR), pig slurry (PS), anaerobically digested pig slurry (ADS) and composted pig slurry (CS), besides a control without fertilization (CTR). Soil samples were collected in the 0-5, 5-10, 10-20, 20-30, 30-40 and 40-60 cm soil layers in 2017. C and N pools were isolated (Cambardella and Elliott, 1992) and stocks were compared in equivalent soil masses (ESM) (Wendt and Hauser, 2013). POC and PN pools were higher at the 0-5 cm soil layer of NT-CS (10.6 and 0.76 Mg ha-1) in relation to other NT (7.0 and 0.51 Mg ha-1) and CT treatments (3.9 and 0.25 Mg ha-1). The tested N fertilization treatments had no effect on TOC and TN stocks regardless of tillage system and sampling layer. TOC stocks were higher under NT (18.6 and 13.8 Mg C ha-1) than CT (12.4 and 12.4 Mg C ha-1) at the both 0-5 and 5-15 cm soil layers, respectively. The same soil layers also had higher TN stocks under NT (1.53 and 1.19 Mg N ha-1) than CT (1.04 and 1.04 Mg N ha-1). Differences observed at the soil surface were sustained throughout the whole profile (0-60 cm), where TOC and TN stocks were 8.2 and 0.82 Mg ha-1 higher in NT in comparison with CT.

    See more from this Division: SSSA Division: Soil and Water Management and Conservation
    See more from this Session: Soil and Water Management and Conservation General Poster III