2015
DOI: 10.2136/sssaspecpub61.c3
|View full text |Cite
|
Sign up to set email alerts
|

Synchrotron X-Ray Microtomography-New Means to Quantify Root Induced Changes of Rhizosphere Physical Properties

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
3
0

Year Published

2015
2015
2021
2021

Publication Types

Select...
4
1

Relationship

0
5

Authors

Journals

citations
Cited by 7 publications
(3 citation statements)
references
References 120 publications
0
3
0
Order By: Relevance
“…Carminati et al (2009) used X-ray CT to observe the dynamics of air gaps at a 90-μm resolution in the white lupin rhizosphere in response to wetting and drying cycles. Recent work of Aravena et al (2013) measured compaction and provided new insights into soil-water uptake in sweet pea (Lathyrus odoratus) and sunflower (Helianthus annuus) using a 4.4-μm resolution CT technique.…”
Section: Imaging Techniquesmentioning
confidence: 99%
“…Carminati et al (2009) used X-ray CT to observe the dynamics of air gaps at a 90-μm resolution in the white lupin rhizosphere in response to wetting and drying cycles. Recent work of Aravena et al (2013) measured compaction and provided new insights into soil-water uptake in sweet pea (Lathyrus odoratus) and sunflower (Helianthus annuus) using a 4.4-μm resolution CT technique.…”
Section: Imaging Techniquesmentioning
confidence: 99%
“…Furthermore, soil pore size distribution is an important soil physical property in relation to root development through their effect on mechanical resistance (Hosseini et al 2016). Some studies have shown that the growth of roots modifies the physical environment by moving soil particles, deforming aggregates and decreasing the number of interaggregate pores (Aravena et al 2013;Pagenkemper et al 2013). The presence of soil macropores significantly benefits root growth (Bennie 1991) because continuous macropores can positively affect the flow of water and nutrients to roots (Hatano et al 1988;Chapman and Miller 2011).…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, root-induced macropores are generated mainly within the compact soil layer (Lesturgez et al 2004;Pfeifer et al 2015). In addition, growing roots modify the physical properties of the rhizosphere (Aravena et al 2013), resulting in significant improvements of the macroporosity and intraaggregate porosity of this compact layer (Lesturgez et al 2004). However, the effects of root growth on the soil structure, especially on the three-dimensional (3-D) macropore characteristics, remain poorly understood in alpine environments.…”
Section: Introductionmentioning
confidence: 99%