Aggregate hierarchy and carbon mineralization in two Oxisols of New South Wales, Australia

被引:47
|
作者
Rabbi, S. M. Fazle [1 ,2 ]
Wilson, Brian R. [1 ,3 ]
Lockwood, Peter V. [1 ]
Daniel, Heiko [1 ]
Young, Iain M. [1 ]
机构
[1] Univ New England, Sch Environm & Rural Sci, Armidale, NSW 2351, Australia
[2] Khulna Univ, Soil Sci Discipline, Khulna 9208, Bangladesh
[3] NSW Off Environm & Heritage, Armidale, NSW 2351, Australia
来源
SOIL & TILLAGE RESEARCH | 2015年 / 146卷
关键词
Macro-aggregates; Micro-aggregates; Organic carbon; Carbon mineralization; Pore geometry; SOIL ORGANIC-MATTER; COMPUTED-TOMOGRAPHY; SIZE FRACTIONS; QUANTIFICATION; MECHANISMS; STORAGE;
D O I
10.1016/j.still.2014.10.008
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The conventional model of aggregate formation suggests a hierarchy where micro-aggregates with lower porosity and therefore reduced soil organic carbon (SOC) mineralization form inside macro-aggregates. This model has however been questioned for highly weathered Oxisols where inconclusive results regarding the presence of aggregate hierarchy have been obtained to date. We hypothesized that in Oxisols (i) an aggregate hierarchy would be present (ii) the porosity of micro-aggregates would be lower than that of macro-aggregates and (iii) pore geometry of aggregates would influence SOC mineralization. We collected topsoils from Oxisols in northern New South Wales, Australia from which macro-aggregates (>250 mu m), micro-aggregates (53-250 mu m) and <53 mu m fractions were isolated from bulk soil by wet sieving. 3D images of macro- and micro-aggregates were produced using X-ray computed tomography (mu CT) showing the presence of micro-aggregates inside macro-aggregates, which confirmed the presence of an aggregate hierarchy in the Oxisols studied. Macro-aggregates were more common and SOC in higher concentrations in forest systems compared with agricultural (the cultivation or pasture) land-uses, but aggregate geometry differed little between the land-uses studied. The porosity of macroaggregates (4%) was significantly lower than micro-aggregates (5.5%). Despite the differences in pore geometry between macro- and micro-aggregates, SOC mineralized (SOCmin) during a 2-month incubation (at 25 degrees C) was similar in macro- (3% of SOC concentration) and micro-aggregates (2.8% of SOC concentration). We conclude that although aggregate hierarchy exists in these soils and that aggregate geometry did differ between aggregate size classes, there was no evidence to support the porosity exclusion principle and the assumption that SOC is preferentially stabilized within microaggregates in these soils. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:193 / 203
页数:11
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