139-4 Application of a Laser Diffraction Technique to Measure Water Stable Soil Aggregates in Response to Agricultural Landuse in Ile-Ife, Nigeria.

See more from this Division: SSSA Division: Soil & Water Management & Conservation
See more from this Session: Management Impacts on Soil Properties and Soil C and N Dynamics: I
Monday, November 3, 2014: 9:15 AM
Hyatt Regency Long Beach, Shoreline A
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Durodoluwa Joseph Oyedele1, Roberto Pini2, Manuel Scatena2, Enzo Sparvolli2 and Oladapo Fatai Tijani3, (1)Obafemi Awolowo University, Ile-Ife, NIGERIA
(2)Institute for Soil Ecosystem - National Centre for Research (ISE-CNR), Pisa, Italy
(3)Obafemi Awolowo University, Ile Ife, Nigeria
The Mastersizer 2000G (Malvern Instruments) Diffraction Instrument was used to assess and quantify the breakdown of soil aggregates and compute wet aggregate stability indices.  The study was aimed at evolving a novel rapid method for determining soil aggregate stability. Bulk surface (0-15 cm) soil samples were collected under 5 different land uses in the Teaching and Research Farm of the Obafemi Awolowo University, Ile-Ife, Nigeria. About 0.5g of the soils aggregates (0.5 -1 mm diameter) were evaluated in the laser diffraction equipment with the stirrer operated at 500 rpm and the pump at 1800 rpm. The different size aggregates and particles of sand silt and clay were quantified periodically. Water stable aggregates greater than 250 µm (WSA>250), water stable aggregates less than 250 µm (WSA<250), water dispersible clay index (WDI), and mean volume diameter (MVD) among others were computed from the laser diffraction data. The values were compared with the classical Yoder wet sieving technique. The WSA>250 was significantly higher on the soils under Forest (FR), Cacao (CC), Teak (TK) and Oil Palm (OP) plantations, while it was significantly lowest in the cultivated plots (no-tillage (NT) and conventional cultivation (CT)). The pasture (PD) was not significantly different from either the cultivated or the non-cultivated soils. Conversely, the WSA<250 and water dispersible clay index were highest in the cultivated soils (CT and NT) and lowest in the non-cultivated soils (FR, TK, CC and OP) while the PD was in-between. The MVD followed a similar trend as the WSA>250. The Yoder wet sieving water stable aggregates index (WSI>250) was significantly correlated with WSA>250 (r = 0.75), MVD (r = 0.75), WDI (r = -0.68) and WSA<250 (r = - 0.73). All the laser diffraction measured aggregation indices were significantly correlated with the organic matter contents of the soils. Thus the laser diffraction promises a rapid and comprehensive method of evaluation of soil aggregate stability.
See more from this Division: SSSA Division: Soil & Water Management & Conservation
See more from this Session: Management Impacts on Soil Properties and Soil C and N Dynamics: I