Pore, live root and necromass quantification in complex heterogeneous wetland soils using X-ray computed tomography

被引:13
作者
Chirol, Clementine [1 ]
Carr, Simon J. [1 ,2 ]
Spencer, Kate L. [1 ]
Moeller, Iris [1 ,3 ]
机构
[1] Queen Mary Univ London, Sch Geog, Mile End Rd, London E1 4NS, England
[2] Univ Cumbria, Inst Sci, Nat Resources & Outdoor Studies, Ambleside LA22 9BB, Cumbria, England
[3] Trinity Coll Dublin, Sch Geog, Dublin 2, Ireland
关键词
X-ray computed tomography; Sediment; Microstructure; Porosity; Live roots; Necromass; Soil carbon dynamics; GREENHOUSE-GAS EMISSIONS; SYSTEM ARCHITECTURE; SEDIMENT STRUCTURE; CARBON; MICROTOMOGRAPHY; ENVIRONMENT; DEFORMATION; BIOMASS; MODEL; EARTH;
D O I
10.1016/j.geoderma.2020.114898
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Subsurface structures and especially the interactions between pores, roots and other organic matter elements have a strong impact on ecosystem functioning. Yet despite recent progress in the application of X-ray Computed Microtomography (mu CT) to soil structure in agricultural science, applications to the more complex and heterogeneous substrates found in natural soils, specifically wetland soils, remain sparse. We apply X-ray mu CT to a complex hetemgenous soil and develop a robust segmentation method to quantify the pores, live roots and necromass. This approach significantly improves the detection of the organic matter elements, and gives us unprecedented detail and resolution in the segmentation of pores, live roots and necromass at a high spatial resolution (62.5 mu m in this study). We identify several situations where pores and organic matter interact in the soil, including the disconnected air spaces (aerenchyma) that run within the Spartina stem and roots, tubularshaped pores left behind by decaying roots, and lateral roots deploying within structural fragilities in the sediment. The capacity of X-ray mu CT to distinguish the connected live root system from the necmmass opens possibilities for applications to determine key wetland soil functions such as soil cohesivity, soil nutrient exchanges and soil carbon dynamics.
引用
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页数:13
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