Spatial Variability of Orange Spotting Disease in Oil Palm

2012 ◽  
Vol 12 (4) ◽  
pp. 232-238 ◽  
Author(s):  
S. Selvaraja ◽  
S.K. Balasundra ◽  
G. Vadamalai ◽  
M.H.A. Husni
Keyword(s):  
2010 ◽  
Vol 5 (4) ◽  
pp. 252-262
Author(s):  
M.C. Law ◽  
S.K. Balasundra ◽  
M.H.A. Husni ◽  
O.H. Ahmed ◽  
Mohd. Hanif Haru

2006 ◽  
Vol 5 (2) ◽  
pp. 397-408 ◽  
Author(s):  
S.K. Balasundra ◽  
P.C. Robert . ◽  
D.J. Mulla . ◽  
D.L. Allan .

2009 ◽  
Vol 4 (12) ◽  
pp. 402-417 ◽  
Author(s):  
M.C. Law ◽  
S.K. Balasundra ◽  
M.H.A. Husni ◽  
O.H. Ahmed ◽  
Mohd. Haniff Har

2008 ◽  
Vol 5 (9) ◽  
pp. 1239-1246 ◽  
Author(s):  
Abdul Rahim Anuar ◽  
Kah Joh Goh ◽  
Tee Bee Heoh ◽  
Osumanu Haruna Ahmed

Soil Research ◽  
2016 ◽  
Vol 54 (4) ◽  
pp. 397 ◽  
Author(s):  
Iain Goodrick ◽  
Paul N. Nelson ◽  
Steven Nake ◽  
Michael J. Webb ◽  
Michael I. Bird ◽  
...  

Soil carbon fluxes are highly variable in space and time under tree crops such as oil palm, and attempts to model such fluxes must incorporate an understanding of this variability. In this work, we measured soil CO2 emission, root biomass and pruned frond deposition rates and calculated carbon fluxes into and out of the soil in a mature (20-year-old, second planting cycle) oil palm plantation in Papua New Guinea. Tree-scale spatial variability in CO2 emission and root biomass was quantified by making measurements on a 35-point trapezoid grid covering the 38.5-m2 repeating unit of the plantation (n = 4 grids). In order to obtain an overall mean soil CO2 emission rate within 5% of the most accurate estimate, ≥24 measurement points were required. Soil CO2 emissions were spatially correlated with calculated carbon inputs (r2 = 0.605, slope 1 : 1), but not with soil water content or temperature. However, outputs were higher than inputs at all locations, with a mean overall output of 7.24 µmol m–2 s–1 and input of 3.02 µmol m–2 s–1. Inputs related to fronds, roots and groundcover constituted 60%, 36% and 4% of estimated inputs, respectively. The spatial correlation of carbon inputs and outputs indicates that mineralisation rate is controlled mostly by the amount rather than the nature or input depth of the additions. The spatially uniform net carbon emission from soil may be due to inaccuracies in calculated fluxes (especially root-related inputs) or to non-biological emissions.


Solid Earth ◽  
2016 ◽  
Vol 7 (3) ◽  
pp. 979-993 ◽  
Author(s):  
Sanjib Kumar Behera ◽  
Kancherla Suresh ◽  
Bezawada Narsimha Rao ◽  
Ravi Kumar Mathur ◽  
Arvind Kumar Shukla ◽  
...  

Abstract. Mapping spatial variability of soil properties is the key to efficient soil resource management for sustainable crop yield. Therefore, the present study was conducted to assess the spatial variability of soil properties such as acidity (pH), salinity (electrical conductivity (EC)), organic carbon, available K, available P, exchangeable Ca2+, exchangeable Mg2+, available S and hot water soluble B in surface (0–20 cm) and subsurface (20–40 cm) soil layers of oil palm plantations in south Goa district of Goa located in west coastal area of India. A total of 128 soil samples were collected from 64 oil palm plantations of Goa located at an approximate interval of 1–2 km and analyzed. Soil was acidic to neutral in reaction. Other soil properties varied widely in both the soil layers. Correlations between soil pH and exchangeable Ca2+, between soil EC and available K, between available P and available S and between exchangeable Ca2+ and exchangeable Mg2+ in both the soil layers were found to be positive and significant (P < 0.01). Geostatistical analysis revealed a varied spatial distribution pattern for the measured soil properties. Best-fit models for measured soil properties were exponential, Gaussian, stable, K-Bessel and spherical with moderate to strong spatial dependency. The results revealed that site-specific fertilizer management options needed to be adopted in the oil palm plantations of the study area owing to variability in soil properties.


2006 ◽  
Vol 1 (3) ◽  
pp. 184-195 ◽  
Author(s):  
S.K. Balasundra ◽  
D.J. Mulla ◽  
P.C. Robert ◽  
D.L. Allan

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