Soil organic carbon and mineral interactions on climatically different hillslopes

Xiang Wang, Kyungsoo Yoo, Adrian A. Wackett, Jessica L Gutknecht, Ronald Amundson, Arjun Heimsath

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

Climate and topography have been widely recognized but studied separately as important factors controlling soil organic carbon (SOC) dynamics. Subsequently, the significance of their interplay in determining SOC storages and their pools is not well understood. Here we examined SOC storages and SOC-mineral interactions along two hillslope transects in differing climate zones (MAP = 549 mm in semi-arid eucalyptus savannah vs. 816 mm in temperate eucalyptus forest) in southeastern Australia. On eroding slopes, SOC inventories were twice as large at the wetter site (4.5 ± 0.6 vs. 2.3 ± 0.9 kg m−2), whereas depositional soils had similar SOC inventories at both locations (7.5 ± 2.0 vs.7.0 ± 2.2 kg m−2). On eroding slopes, carbon concentrations of the mineral-associated SOC fraction (<250 μm and >2.0 g cm−3) increased by ~50% with increasing rainfall, which was also positively correlated to abundances of clay minerals and pedogenic iron oxides. Within individual hillslopes, carbon concentrations of the mineral-associated SOC fraction doubled from eroding to depositional soils at the drier site, but no topographic trend was observed at the wetter site. The effects of topography on SOC inventories and mineral-associated SOC were more strongly expressed under the drier climate, where vegetation was sparser and soil erosion involved mineral grain size sorting. Our results demonstrate that SOC pools and their interactions with minerals are dependent on topographic locations, emphasizing the need to include geomorphic data when assessing climatic controls of SOC.

Original languageEnglish (US)
Pages (from-to)71-80
Number of pages10
JournalGeoderma
Volume322
DOIs
StatePublished - Jul 15 2018

Fingerprint

hillslope
soil organic carbon
organic carbon
minerals
mineral
soil
carbon footprint
carbon sequestration
Eucalyptus
mineral content
topography
climate
carbon
iron oxides
clay minerals
carbon sinks
soil erosion
sorting
savannas
temperate forest

Keywords

  • Bioturbation
  • Climate
  • Erosion
  • Microclimate
  • Mineral associated organic carbon
  • Soil carbon
  • Topography

Cite this

Soil organic carbon and mineral interactions on climatically different hillslopes. / Wang, Xiang; Yoo, Kyungsoo; Wackett, Adrian A.; Gutknecht, Jessica L; Amundson, Ronald; Heimsath, Arjun.

In: Geoderma, Vol. 322, 15.07.2018, p. 71-80.

Research output: Contribution to journalArticle

Wang, Xiang ; Yoo, Kyungsoo ; Wackett, Adrian A. ; Gutknecht, Jessica L ; Amundson, Ronald ; Heimsath, Arjun. / Soil organic carbon and mineral interactions on climatically different hillslopes. In: Geoderma. 2018 ; Vol. 322. pp. 71-80.
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