REDUCING NITROGEN LOSSES AND INCREASING MAIZE PRODUCTIVITY IN ORGANIC MANURES-AMENDED SOILS BY INCREASING THE RIDGE TO FURROW PROPORTION

2018 ◽  
Vol 55 (3) ◽  
pp. 428-442 ◽  
Author(s):  
SHAHID IQBAL ◽  
MUHAMMAD ARIF ◽  
CHRISTIAN THIERFELDER ◽  
TAHIRA YASMEEN ◽  
TANG LI

SUMMARYNitrogen (N) losses greater than 40% in furrow-irrigated cropping systems are a common problem that substantially limits yields. Sustainable production methods are therefore required to reduce these losses and increase the yield under semi-arid conditions. A field trial was carried out to study the soil N dynamics and soil physicochemical properties in soils amended with organic manure (i.e. with poultry manure (PM), farmyard manure (FYM) and pressmud compost (PrM)). Soil N dynamics and properties were evaluated under different ridge to furrow ratios (1:1 and 2:1) as well as maize yield and profitability. When ridge to furrow ratio increased (2:1) in soils amended with PM, the inorganic and organic N status was increased and N losses were reduced. This strategy lowered soil pH, and maximized organic matter status and maize yield. The highest yield, net income and benefit–cost ratio were attained with 2:1 ridge to furrow ratio and PM amendment, being an alternative management for increasing maize productivity and profitability while improving nutrient use efficiency.

2005 ◽  
Vol 75 (1) ◽  
pp. 65-80 ◽  
Author(s):  
A. K. Patra ◽  
L. Abbadie ◽  
A. Clays-Josserand ◽  
V. Degrange ◽  
S. J. Grayston ◽  
...  

1998 ◽  
Vol 27 (3) ◽  
pp. 267-273 ◽  
Author(s):  
N. Jamieson ◽  
D. Barraclough ◽  
M. Unkovich ◽  
R. Monaghan

2007 ◽  
Vol 103 (2) ◽  
pp. 98-108 ◽  
Author(s):  
M. Becker ◽  
F. Asch ◽  
S.L. Maskey ◽  
K.R. Pande ◽  
S.C. Shah ◽  
...  

1994 ◽  
Vol 24 (8) ◽  
pp. 1636-1645 ◽  
Author(s):  
Charles T. Garten Jr. ◽  
Helga Van Miegroet

We tested the hypothesis that naturally occurring nitrogen (N) isotope ratios in foliage (from plants that do not symbiotically fix atmospheric N2) are an indicator of soil N dynamics in forests. Replicate plots were established at eight locations ranging in elevation from 615 to 1670 m in Great Smoky Mountains National Park in eastern Tennessee, U.S.A. The locations selected ranged from N-poor (low-elevation) to N-rich (high-elevation) forest stands. Soils were sampled in June 1992; plants, forest floors, and upper mineral soils were sampled in August 1992. Net N mineralization and net nitrification potentials for surface mineral soils and organic matter layers at each site were determined by aerobic laboratory incubations. Soils and organic layers from high-elevation sites had greater net N mineralization and nitrification potentials than soils from low-elevation sites. There were significant (P ≤ 0.05) differences between study sites in soil 15N abundance. Therefore, we examined correlations between measures of soil N availability and both mean foliar δ15N values and mean enrichment factors (εp−s = δ15Nleaf − δ15Nsoil). In evergreens, maples, and ferns, mean foliar δ15N values and mean enrichment factors were positively correlated with net N mineralization and net nitrification potentials in soil. The observed relationships between natural 15N abundance in plant leaves and soil N availability were explained by a simple model of soil N dynamics. The model predicts how the isotopic composition of plant N is affected by the following factors: (i) varying uptake of soil NH4-N and NO3-N, (ii) the isotopic composition of different soil N pools, and (iii) relative rates of soil N transformations.


2015 ◽  
Vol 91 ◽  
pp. 222-231 ◽  
Author(s):  
Jing Wang ◽  
Bo Zhu ◽  
Jinbo Zhang ◽  
Christoph Müller ◽  
Zucong Cai

2000 ◽  
Vol 137 (1-3) ◽  
pp. 41-51 ◽  
Author(s):  
L.J. Ellingson ◽  
J.B. Kauffman ◽  
D.L. Cummings ◽  
R.L. Sanford ◽  
V.J. Jaramillo

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