Details
Original language | English |
---|---|
Pages (from-to) | 31-39 |
Number of pages | 9 |
Journal | GEODERMA |
Volume | 245-246 |
Publication status | Published - 1 May 2015 |
Abstract
Adding carbon-rich solids from pyrolysis (pyrochars) and hydrothermal carbonization (hydrochars) to soils can improve their hydraulic properties and increase the plant available soil water capacity (AWC). However, the effects of the specific char characteristics on soil hydraulic properties are still little understood and thus, difficult to optimize for soil amendment. It is often assumed that the water repellency of chars is an important factor influencing the water retention of soils. In using the evaporation method and saturated conductivity measurements, we investigated how changes of hydraulic properties of a loamy sand with 2% (w/w) char addition depend on (i) production processes, (ii) feedstocks, (iii) particle size, and (iv) wetting properties of added chars. Applied chars comprised pyrochars carbonized at 750. °C and hydrochars carbonized at 200. °C and 250. °C from two different feedstocks (digestate and woodchips) and two particle sizes (<. 0.5. mm and 0.5-1.0. mm). The wetting properties of the pure chars and soil-char composites were determined by the sessile drop method. To investigate the impact of the water repellency of chars, pure chars and soil-char composites were saturated by capillary water uptake under atmospheric conditions and by saturation from the bottom under vacuum conditions.The chars showed highly variable wetting properties with the contact angles being strongly correlated to the specific surface area of the chars. The saturated hydraulic conductivity was significantly increased after char addition for both vacuum and capillary saturated samples, while being independent of wettability characteristics. The effects for the unsaturated conductivity were negligible. In contrast to expectation, soil amendments with more water repellent chars caused higher increases of AWC (up to 15%), both after vacuum and capillary saturated conditions. Highest increase of AWC occurred for chars from digestate material, particle size fractions <. 0.5. mm, and chars hydrothermally carbonized at 200. °C. The increase of AWC only occurred in the low pressure range (pF. 1.8 to 2.5), whereas it was decreased in the high pressure range (pF. 2.5 to 4.2). Our study indicates that water repellency of pyrochars and hydrochars have little counteracting effect on the overall improvement of soil water retention and saturated conductivity, and other factors that also depend on production process and feedstock, such as particle size, intra-particle porosity, shape, and plasticity are more important.
Keywords
- Biochar, Contact angle, Hydraulic conductivity, Hydrophobicity, Hydrothermal carbonization, Pyrolysis, Water retention
ASJC Scopus subject areas
- Agricultural and Biological Sciences(all)
- Soil Science
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In: GEODERMA, Vol. 245-246, 01.05.2015, p. 31-39.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Does water repellency of pyrochars and hydrochars counter their positive effects on soil hydraulic properties?
AU - Eibisch, Nina
AU - Durner, Wolfgang
AU - Bechtold, Michel
AU - Fuß, Roland
AU - Mikutta, Robert
AU - Woche, Susanne K.
AU - Helfrich, Mirjam
N1 - Publisher Copyright: © 2015 Elsevier B.V. Copyright: Copyright 2015 Elsevier B.V., All rights reserved.
PY - 2015/5/1
Y1 - 2015/5/1
N2 - Adding carbon-rich solids from pyrolysis (pyrochars) and hydrothermal carbonization (hydrochars) to soils can improve their hydraulic properties and increase the plant available soil water capacity (AWC). However, the effects of the specific char characteristics on soil hydraulic properties are still little understood and thus, difficult to optimize for soil amendment. It is often assumed that the water repellency of chars is an important factor influencing the water retention of soils. In using the evaporation method and saturated conductivity measurements, we investigated how changes of hydraulic properties of a loamy sand with 2% (w/w) char addition depend on (i) production processes, (ii) feedstocks, (iii) particle size, and (iv) wetting properties of added chars. Applied chars comprised pyrochars carbonized at 750. °C and hydrochars carbonized at 200. °C and 250. °C from two different feedstocks (digestate and woodchips) and two particle sizes (<. 0.5. mm and 0.5-1.0. mm). The wetting properties of the pure chars and soil-char composites were determined by the sessile drop method. To investigate the impact of the water repellency of chars, pure chars and soil-char composites were saturated by capillary water uptake under atmospheric conditions and by saturation from the bottom under vacuum conditions.The chars showed highly variable wetting properties with the contact angles being strongly correlated to the specific surface area of the chars. The saturated hydraulic conductivity was significantly increased after char addition for both vacuum and capillary saturated samples, while being independent of wettability characteristics. The effects for the unsaturated conductivity were negligible. In contrast to expectation, soil amendments with more water repellent chars caused higher increases of AWC (up to 15%), both after vacuum and capillary saturated conditions. Highest increase of AWC occurred for chars from digestate material, particle size fractions <. 0.5. mm, and chars hydrothermally carbonized at 200. °C. The increase of AWC only occurred in the low pressure range (pF. 1.8 to 2.5), whereas it was decreased in the high pressure range (pF. 2.5 to 4.2). Our study indicates that water repellency of pyrochars and hydrochars have little counteracting effect on the overall improvement of soil water retention and saturated conductivity, and other factors that also depend on production process and feedstock, such as particle size, intra-particle porosity, shape, and plasticity are more important.
AB - Adding carbon-rich solids from pyrolysis (pyrochars) and hydrothermal carbonization (hydrochars) to soils can improve their hydraulic properties and increase the plant available soil water capacity (AWC). However, the effects of the specific char characteristics on soil hydraulic properties are still little understood and thus, difficult to optimize for soil amendment. It is often assumed that the water repellency of chars is an important factor influencing the water retention of soils. In using the evaporation method and saturated conductivity measurements, we investigated how changes of hydraulic properties of a loamy sand with 2% (w/w) char addition depend on (i) production processes, (ii) feedstocks, (iii) particle size, and (iv) wetting properties of added chars. Applied chars comprised pyrochars carbonized at 750. °C and hydrochars carbonized at 200. °C and 250. °C from two different feedstocks (digestate and woodchips) and two particle sizes (<. 0.5. mm and 0.5-1.0. mm). The wetting properties of the pure chars and soil-char composites were determined by the sessile drop method. To investigate the impact of the water repellency of chars, pure chars and soil-char composites were saturated by capillary water uptake under atmospheric conditions and by saturation from the bottom under vacuum conditions.The chars showed highly variable wetting properties with the contact angles being strongly correlated to the specific surface area of the chars. The saturated hydraulic conductivity was significantly increased after char addition for both vacuum and capillary saturated samples, while being independent of wettability characteristics. The effects for the unsaturated conductivity were negligible. In contrast to expectation, soil amendments with more water repellent chars caused higher increases of AWC (up to 15%), both after vacuum and capillary saturated conditions. Highest increase of AWC occurred for chars from digestate material, particle size fractions <. 0.5. mm, and chars hydrothermally carbonized at 200. °C. The increase of AWC only occurred in the low pressure range (pF. 1.8 to 2.5), whereas it was decreased in the high pressure range (pF. 2.5 to 4.2). Our study indicates that water repellency of pyrochars and hydrochars have little counteracting effect on the overall improvement of soil water retention and saturated conductivity, and other factors that also depend on production process and feedstock, such as particle size, intra-particle porosity, shape, and plasticity are more important.
KW - Biochar
KW - Contact angle
KW - Hydraulic conductivity
KW - Hydrophobicity
KW - Hydrothermal carbonization
KW - Pyrolysis
KW - Water retention
UR - http://www.scopus.com/inward/record.url?scp=84921449471&partnerID=8YFLogxK
U2 - 10.1016/j.geoderma.2015.01.009
DO - 10.1016/j.geoderma.2015.01.009
M3 - Article
AN - SCOPUS:84921449471
VL - 245-246
SP - 31
EP - 39
JO - GEODERMA
JF - GEODERMA
SN - 0016-7061
ER -