2019
DOI: 10.1007/978-981-13-5767-1_10
|View full text |Cite
|
Sign up to set email alerts
|

Using a Tri-Isotope (13C, 15N, 33P) Labelling Method to Quantify Rhizodeposition

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3

Citation Types

0
3
0

Year Published

2020
2020
2024
2024

Publication Types

Select...
3
1
1

Relationship

0
5

Authors

Journals

citations
Cited by 5 publications
(3 citation statements)
references
References 96 publications
0
3
0
Order By: Relevance
“…4). This simplification is made because of the difficulties in measuring quantitative characteristics of rhizodeposits in a soil medium (Oburger and Jones, 2018) but leads to erroneous calculations of the amount of carbon rhizodeposition when this assumption is violated (Stevenel et al, 2019). To assess the uncertainty of calculated values of subsoil carbon sequestration, we calculated how these values differ when the value of root δ 13 C is varied with ±25 % (Fig.…”
Section: Rates Of Net Carbon Rhizodepositionmentioning
confidence: 99%
“…4). This simplification is made because of the difficulties in measuring quantitative characteristics of rhizodeposits in a soil medium (Oburger and Jones, 2018) but leads to erroneous calculations of the amount of carbon rhizodeposition when this assumption is violated (Stevenel et al, 2019). To assess the uncertainty of calculated values of subsoil carbon sequestration, we calculated how these values differ when the value of root δ 13 C is varied with ±25 % (Fig.…”
Section: Rates Of Net Carbon Rhizodepositionmentioning
confidence: 99%
“…calculations of the amount of carbon rhizodeposition when this assumption is violated (Stevenel et al, 2019). The latter is likely to be the case for two main reasons.…”
Section: Rates Of Net Carbon Rhizodepositionmentioning
confidence: 99%
“…Second, the fact that most carbon is allocated to belowground plant parts during the first 1 to months after growth initiation (Pausch and Kuzyakov, 2018) likely causes an important temporal variation in the 13 C enrichment of roots. Recently, Stevenel et al (2019) have shown that the δ 13 C value of roots of isotopically labeled Canavalia brasiliensis differed both temporally and spatially, as different parts of the root had a different isotopic value at the end of their 22-day experiment.…”
Section: Rates Of Net Carbon Rhizodepositionmentioning
confidence: 99%