2021
DOI: 10.1007/s11368-020-02850-6
|View full text |Cite
|
Sign up to set email alerts
|

Genetic and environmental influence on foliar carbon isotope composition, nitrogen availability and fruit yield of 5-year-old mango plantation in tropical Australia

Abstract: The aim of this study was to quantify the effect of different varieties, planting densities, tree training systems and canopy aspect (north and south) on tree water use efficiency and nitrogen (N) availability in relation to mango fruit yield and fruit size as well as soil fertility (particularly total carbon (C) and total N as well as C and N isotope compositions) in a 5-year-old mango plantation of tropical Australia. Material and Methods Mango foliar samples were collected from a 5-year-old, factorial field… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2021
2021
2024
2024

Publication Types

Select...
4

Relationship

1
3

Authors

Journals

citations
Cited by 4 publications
(1 citation statement)
references
References 108 publications
0
1
0
Order By: Relevance
“…Thus, higher δ 15 N in terrestrial ecosystems indicates active N cycling or N availability because of increased microbial activity (Asadyar et al., 2021; Hosseini‐Bai et al., 2015; Succarie et al., 2022; Wang et al., 2020). On the other hand, soil δ 13 C is a biological indicator of C cycling and could be used to interpret soil organic matter (SOM) mineralization processes and land uses (Wang et al., 2013; Saiz et al., 2016; Succarie et al., 2020; Sun et al., 2021; Liu et al., 2021; Fu et al., 2023). The C cycle is vital because it affects soil respiration and the process of plant photosynthesis (Farooq et al., 2021; Liu et al., 2021; Succarie et al., 2020; Fu et al., 2023).…”
Section: Introductionmentioning
confidence: 99%
“…Thus, higher δ 15 N in terrestrial ecosystems indicates active N cycling or N availability because of increased microbial activity (Asadyar et al., 2021; Hosseini‐Bai et al., 2015; Succarie et al., 2022; Wang et al., 2020). On the other hand, soil δ 13 C is a biological indicator of C cycling and could be used to interpret soil organic matter (SOM) mineralization processes and land uses (Wang et al., 2013; Saiz et al., 2016; Succarie et al., 2020; Sun et al., 2021; Liu et al., 2021; Fu et al., 2023). The C cycle is vital because it affects soil respiration and the process of plant photosynthesis (Farooq et al., 2021; Liu et al., 2021; Succarie et al., 2020; Fu et al., 2023).…”
Section: Introductionmentioning
confidence: 99%