Combined turnover of carbon and soil aggregates using rare earth oxides and isotopically labelled carbon as tracers

Xinhua Peng (Corresponding Author), Qiaohong Zhu, Zhongbin Zhang, Paul Hallett

Research output: Contribution to journalArticle

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Abstract

This study used a combined tracer approach of isotopically labelled carbon (C) and rare earth oxides (REO) to determine soil aggregate transfer paths following input of organic matter. A model quantifying aggregate turnover rates over time was verified by a controlled incubation study. Four natural soil aggregate size ranges (<0.053 mm, 0.053-0.25 mm, 0.25-2 mm and 2-5 mm) were labelled with different REO tracers and packed to form a composite soil sample. The organic input was 1 mg 13C g-1 soil of 13C-labelled glucose. There were four treatments: i) soil without REO and 13C as a control, ii) soil labelled with REO, iii) soil without REO but amended with 13C-glucose, and iv) soil labelled with REO and amended with 13C-glucose. Aggregate stability, REO concentrations, soil respiration and 13C were measured after 0, 7, 14 and 28 days incubation. REOs were found to not impact microbial activity (P > 0.05). Based on the 84%-106% recovery of REOs after wet sieving of aggregates, and a close 1:1 relationship between measured aggregates and model predictions, REOs were found to be an effective tracer for studies of aggregate dynamics. A greater portion of aggregates transferred between neighbouring size fractions. The turnover rate was faster for macroaggregates than for microaggregates, and slowed down over the incubation time. The new C was accumulated more but decomposed faster in macroaggregates than in microaggregates. A positive relationship was observed between the 13C concentration in aggregates and the aggregate turnover rate (P < 0.05). The relative change in each aggregate fraction generally followed an exponential growth over time in the formation direction and an exponential decay in the breakdown direction. We proposed a first order kinetic model for aggregate dynamics which can separate aggregate formation, stabilization and breakdown processes. This study demonstrates that REOs can track aggregate life cycles and provide unique and important information about the relationship between C cycling and aggregate turnover.
Original languageEnglish
Pages (from-to)81-94
Number of pages14
JournalSoil Biology and Biochemistry
Volume109
Early online date16 Feb 2017
DOIs
Publication statusPublished - Jun 2017

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soil aggregate
soil aggregates
Oxides
oxides
tracer techniques
turnover
Soil
Carbon
tracer
oxide
carbon
glucose
macroaggregate
soil
incubation
Glucose
microaggregates
aggregate stability
soil respiration
soil treatment

Keywords

  • aggregate turnover
  • modelling
  • organic amendment
  • rare earth oxide
  • soil aggregation

Cite this

Combined turnover of carbon and soil aggregates using rare earth oxides and isotopically labelled carbon as tracers. / Peng, Xinhua (Corresponding Author); Zhu, Qiaohong; Zhang, Zhongbin; Hallett, Paul.

In: Soil Biology and Biochemistry, Vol. 109, 06.2017, p. 81-94.

Research output: Contribution to journalArticle

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abstract = "This study used a combined tracer approach of isotopically labelled carbon (C) and rare earth oxides (REO) to determine soil aggregate transfer paths following input of organic matter. A model quantifying aggregate turnover rates over time was verified by a controlled incubation study. Four natural soil aggregate size ranges (<0.053 mm, 0.053-0.25 mm, 0.25-2 mm and 2-5 mm) were labelled with different REO tracers and packed to form a composite soil sample. The organic input was 1 mg 13C g-1 soil of 13C-labelled glucose. There were four treatments: i) soil without REO and 13C as a control, ii) soil labelled with REO, iii) soil without REO but amended with 13C-glucose, and iv) soil labelled with REO and amended with 13C-glucose. Aggregate stability, REO concentrations, soil respiration and 13C were measured after 0, 7, 14 and 28 days incubation. REOs were found to not impact microbial activity (P > 0.05). Based on the 84{\%}-106{\%} recovery of REOs after wet sieving of aggregates, and a close 1:1 relationship between measured aggregates and model predictions, REOs were found to be an effective tracer for studies of aggregate dynamics. A greater portion of aggregates transferred between neighbouring size fractions. The turnover rate was faster for macroaggregates than for microaggregates, and slowed down over the incubation time. The new C was accumulated more but decomposed faster in macroaggregates than in microaggregates. A positive relationship was observed between the 13C concentration in aggregates and the aggregate turnover rate (P < 0.05). The relative change in each aggregate fraction generally followed an exponential growth over time in the formation direction and an exponential decay in the breakdown direction. We proposed a first order kinetic model for aggregate dynamics which can separate aggregate formation, stabilization and breakdown processes. This study demonstrates that REOs can track aggregate life cycles and provide unique and important information about the relationship between C cycling and aggregate turnover.",
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note = "This work was granted by the China-UK jointed Red Soil Critical Zone project from National Natural Science Foundation of China (NSFC: 41571130053, 41371235) and from Natural Environmental Research Council (NERC: Code: NE/N007611/1).",
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AU - Hallett, Paul

N1 - This work was granted by the China-UK jointed Red Soil Critical Zone project from National Natural Science Foundation of China (NSFC: 41571130053, 41371235) and from Natural Environmental Research Council (NERC: Code: NE/N007611/1).

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N2 - This study used a combined tracer approach of isotopically labelled carbon (C) and rare earth oxides (REO) to determine soil aggregate transfer paths following input of organic matter. A model quantifying aggregate turnover rates over time was verified by a controlled incubation study. Four natural soil aggregate size ranges (<0.053 mm, 0.053-0.25 mm, 0.25-2 mm and 2-5 mm) were labelled with different REO tracers and packed to form a composite soil sample. The organic input was 1 mg 13C g-1 soil of 13C-labelled glucose. There were four treatments: i) soil without REO and 13C as a control, ii) soil labelled with REO, iii) soil without REO but amended with 13C-glucose, and iv) soil labelled with REO and amended with 13C-glucose. Aggregate stability, REO concentrations, soil respiration and 13C were measured after 0, 7, 14 and 28 days incubation. REOs were found to not impact microbial activity (P > 0.05). Based on the 84%-106% recovery of REOs after wet sieving of aggregates, and a close 1:1 relationship between measured aggregates and model predictions, REOs were found to be an effective tracer for studies of aggregate dynamics. A greater portion of aggregates transferred between neighbouring size fractions. The turnover rate was faster for macroaggregates than for microaggregates, and slowed down over the incubation time. The new C was accumulated more but decomposed faster in macroaggregates than in microaggregates. A positive relationship was observed between the 13C concentration in aggregates and the aggregate turnover rate (P < 0.05). The relative change in each aggregate fraction generally followed an exponential growth over time in the formation direction and an exponential decay in the breakdown direction. We proposed a first order kinetic model for aggregate dynamics which can separate aggregate formation, stabilization and breakdown processes. This study demonstrates that REOs can track aggregate life cycles and provide unique and important information about the relationship between C cycling and aggregate turnover.

AB - This study used a combined tracer approach of isotopically labelled carbon (C) and rare earth oxides (REO) to determine soil aggregate transfer paths following input of organic matter. A model quantifying aggregate turnover rates over time was verified by a controlled incubation study. Four natural soil aggregate size ranges (<0.053 mm, 0.053-0.25 mm, 0.25-2 mm and 2-5 mm) were labelled with different REO tracers and packed to form a composite soil sample. The organic input was 1 mg 13C g-1 soil of 13C-labelled glucose. There were four treatments: i) soil without REO and 13C as a control, ii) soil labelled with REO, iii) soil without REO but amended with 13C-glucose, and iv) soil labelled with REO and amended with 13C-glucose. Aggregate stability, REO concentrations, soil respiration and 13C were measured after 0, 7, 14 and 28 days incubation. REOs were found to not impact microbial activity (P > 0.05). Based on the 84%-106% recovery of REOs after wet sieving of aggregates, and a close 1:1 relationship between measured aggregates and model predictions, REOs were found to be an effective tracer for studies of aggregate dynamics. A greater portion of aggregates transferred between neighbouring size fractions. The turnover rate was faster for macroaggregates than for microaggregates, and slowed down over the incubation time. The new C was accumulated more but decomposed faster in macroaggregates than in microaggregates. A positive relationship was observed between the 13C concentration in aggregates and the aggregate turnover rate (P < 0.05). The relative change in each aggregate fraction generally followed an exponential growth over time in the formation direction and an exponential decay in the breakdown direction. We proposed a first order kinetic model for aggregate dynamics which can separate aggregate formation, stabilization and breakdown processes. This study demonstrates that REOs can track aggregate life cycles and provide unique and important information about the relationship between C cycling and aggregate turnover.

KW - aggregate turnover

KW - modelling

KW - organic amendment

KW - rare earth oxide

KW - soil aggregation

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EP - 94

JO - Soil Biology and Biochemistry

JF - Soil Biology and Biochemistry

SN - 0038-0717

ER -