The potential of biochar in improving drainage, aeration and maize yields in heavy clay soils

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Date
2018-05-11Author
Obia, Alfred
Mulder, Jan
Hale, Sarah Elizabeth
Nurida, Neneng Laela
Cornelissen, Gerard
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Heavy clay soils are globally widespread but their poor drainage and poor aeration limit their
use for agriculture. This study was designed to test the effect of the amendment of biochar
(BC) from woody shrubs on drainage/saturated hydraulic conductivity (Ksat), soil aeration/air
capacity, available water capacity and biomass and grain yields of maize. In a field experi ment, BC from Gliricidia sepium was applied in planting basins or rip lines at 2.5% and 5%
w/w in addition to a control without BC. The maize biomass and grain yields were higher in
BC treated plots compared to control (p<0.05) during the 2012 and 2013 seasons. There
was no significant difference in the yields between 2.5% and 5% BC treatments (e.g. grain
yield were 6.6 and 8.1 t ha-1 in 2012 and 9.3 and 10.3 t ha-1 in 2013 compared to control with
4.2 and 6.7 t ha-1 in 2012 and 2013, respectively). Soil from the same field site was also
mixed with a similar woody shrub BC from Eupatorium adenophorum in the laboratory at
rates of 2.5%, 5% and 10% BC w/w and a control without BC. The mixtures were then incu bated and subjected to two wet-dry cycles for two weeks. Core samples were taken from the
incubated soil and tested for bulk density, Ksat and pF measurements. Total porosity and
moisture at field capacity and wilting point were 72.3%, 43.7% and 23.7%, respectively, and
not affected by BC amendment (p>0.05). In contrast, bulk density decreased linearly by
0.011±0.002 g cm-3 per percent BC added (p<0.001). Ksat and air capacity of the soil were
288 cm day-1 and 30.9%, respectively falling within the generally accepted optimal range.
Both Ksat and air capacity followed a significant quadratic relation (p<0.05) upon BC addi tion, decreasing at low BC doses, reaching a minimum at 3–5% BC and increasing at higher
doses. Results allowed a partial attribution of the yield increases to changes in soil physical
properties such as changes in bulk density and not clearly to Ksat and air capacity.