Table 5 Impact of biochar application on soil biophysical and chemical properties

From: Use of biomass-derived biochar as a sustainable material for carbon sequestration in soil: recent advancements and future perspectives

Biochar source

Soil type

Effect on soil properties/soil quality changes

Different feedstock types

Different soil types

Increase in soil pH, cation exchange capacity (CEC), available K, Ca and Mg, total N and available P; decrease in Al saturation of acid soils.

Wood charcoal

Anthrosol and Ferralsol

Increase in soil C content, pH value and available P; reduction in leaching of applied fertilizer N, Ca and Mg and lower Al contents.

Eucalyptus logs, maize stover

Clay-loam Oxisol; silt loam

Increase in total N derived from the atmosphere by up to 78%; higher total soil N recovery with biochar addition.

Charcoal site Soil

Haplic Acrisols

Increase in total porosity from 46% to 51% and saturated soil hydraulic conductivity by 88% and reduction in bulk density by 9%.

Peanut hulls, pecan shells, poultry litter

Loamy sand

Biochars produced at higher pyrolysis temperature increased soil pH, while biochar made from poultry litter increased available P and Na.

Wood and peanut shell − Chicken manure − wheat chaff

Sandy soils

Increase in P availability from 163 to 208%, but decreased AMF (arbuscular mycorrhizae fungi) abundances in soils from 43 to 77%.

Wood and manure-derived biochars

Different soil types

Increase the soil’s saturated hydraulic conductivity and plant’s water accessibility, as well as boost the soil’s total N concentration and CEC, improving soil field capacity, and reduce NH4-N leaching.

Manure, corn stover, woods, food waste

Alfisol

Tissue N concentration and uptake decreased with increasing pyrolysis temperature and application rate, but increased K and Na content.

Different biochar sources

Different soil types

Increased crop yield, improved microbial habitat and soil microbial biomass, rhizobia nodulation, plant K tissue concentration, soil pH, soil P, soil K, total soil N, and total soil C compared with control conditions.

Peanut hull

Ultisols

Increased K, Ca, and Mg in the surface soil (0–15 cm). Increased K was reflected in the plant tissue analysis.

Simoca, activated wundowie

Loamy sand −clay

Increased soil microbial activity more in clay than loamy soil

Acacia whole tree green waste

Planosol

Increase in porosity either direct pore contribution, creation of accommodation pores or improved aggregate stability

Wheat straw

Fimi-Orthic Anthrosols

Increase in soil pH, organic carbon, total nitrogen and reduction in yield scaled N2O emissions

  1. Reproduced with permission from ref. 111. Copyright (2017) Elsevier.