Investigation on the effect of biochar addition and the use of pasture species with different rooting systems on soil fertility and carbon storage : a thesis presented in partial fulfilment of the requirements for the degree of Master of Philosophy (MPhil) in Soil Science at the Institute of Agriculture and Environment, Massey University, Palmerston North, New Zealand
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2015
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Massey University
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Abstract
There is a potential to increase soil carbon (C) sequestration in New Zealand pastoral soils,
especially in the subsoils where the soil C stocks have been reported to have a greater C
saturation deficit than the topsoils. Selecting pasture species with deeper root systems will
enhance soil formation at depth and mineral weathering, thus enhancing the potential for soils
to stabilize organic matter (OM). Moreover, the addition of biochar may increase the stable C
pool of soils and provide other additional benefits. Up to the present time few studies have
investigated the potential of biochar to promote root growth and allocation of plant C to the
subsoil. A glasshouse study was carried out to examine the effect of adding a nutrient-rich
biochar at various dose (0, 1.5, 5 and 10 Mg ha–1 without nitrogen (N) fertiliser; 0, 1.5, 10 and
20 Mg ha–1 with N fertiliser at a dose of 113 kg N ha–1) to a sandy soil on plant growth (aboveand
below-ground). The results indicated that, in the absence of N limiting conditions,
biosolids-derived biochar could improve plant biomass yield as a result of the addition of
available P and K. This amendment also caused an increase in plant root length. Subsequently,
a 2-year lysimeter trial was set up to compare changes in C stocks of soils under deep- or
shallow-growing pastures as well as to investigate whether biochar addition below the top 10
cm could promote root growth at depth. For this: i) soil ploughing at cultivation for pasture
establishment was simulated in two different soils (a silt loam soil and a sandy soil) by
inverting the 0–10 and 10–20 cm depth soil layers, and biochar was mixed at a rate of 10 Mg
ha–1 in the buried soil layer, where appropriate; and ii) three pasture types with contrasting
root systems were grown. Distinctive biochars were selected for these two soils so that soilspecific
plant growth limitations could be overcome. In the silt loam, soil inversion resulted in a
net loss of native organic C in the buried horizon under shallow-rooted species, but not under
deep-rooted species. The addition of a C-rich pine biochar (equivalent to 7.6 Mg C ha–1) to this
soil resulted in a net C gain (6–16% over the non-biochar treatment, calculated up to 30 cm; P
< 0.05) in the buried soil layer under all pasture treatments; this overcame the net loss of
native organic C in this horizon under shallow-rooted pastures. In the sandy soil all pasture
species were able to maintain soil C stocks at 10–20 cm depth over time. In this soil, the
exposure of a skeletal and nutrient-depleted soil layer at the surface may have fostered root
growth at depth. The addition of a nutrient-rich biosolids biochar (equivalent to 3.6 Mg C ha–1)
to this soil had no apparent effect on total C stocks. In this 2-year study, none of the biochar
amendments affected either pasture yield or root growth. More research is needed to
understand the mechanisms through which soil C stocks at depth are preserved.
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Biochar, Carbon sequestration, Pasture plants, Environmental aspects, Soil amendments, New Zealand, Research Subject Categories::FORESTRY, AGRICULTURAL SCIENCES and LANDSCAPE PLANNING::Soil science