2015
DOI: 10.5897/ajar2014.8706
|View full text |Cite
|
Sign up to set email alerts
|

Carbon and nitrogen stocks under different management systems in the Paraiban Serto

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2016
2016
2023
2023

Publication Types

Select...
6

Relationship

0
6

Authors

Journals

citations
Cited by 14 publications
(1 citation statement)
references
References 15 publications
0
1
0
Order By: Relevance
“…Unfortunately, the Caatinga dry forest has been driven toward desertification over large areas as soils become deeply depauperated due to superficial erosion (i.e., runoff) and nutrient exportation via crops/livestock (Leal et al, 2005;Vieira et al, 2015). Local depletion of forest regeneration sources, such as seeds, seedlings and resprouts can Caatinga soil 20.00 10 cm Tiessen et al, 1998 Caatinga soil 26.20 10 cm Kauffman et al, 1993 Caatinga soil 4.14 5 cm Schulz et al, 2016 Caatinga soil 17.00 5-60 cm Schulz et al, 2016 Caatinga soil 35.13-46.46 40 cm Barros et al, 2015 Caatinga slash and burn recovering soil 23.15 20 cm Althoff et al, 2018 Caatinga preserved soil 31.85 20 cm Althoff et al, 2018 Deserts and Semi Deserts soil 57.00 Across all horizons Prentice et al, 2001 Tropical Savannas and Grasslands soil 90.00 Across all horizons Prentice et al, 2001 Tropical Forest soil 122.00 Across all horizons Prentice et al, 2001 Temperate Forest soil 147.00 Across all horizons Prentice et al, 2001 Boreal Forest soil 274.00 Across all horizons Prentice et al, 2001 also be important (Tabarelli et al, 2017). Increased aridity (as predicted by climate change models; Torres et al, 2017) can magnify this human-induced degradation.…”
Section: Biocrusts As Ecosystem Service Providers and Their Role For mentioning
confidence: 99%
“…Unfortunately, the Caatinga dry forest has been driven toward desertification over large areas as soils become deeply depauperated due to superficial erosion (i.e., runoff) and nutrient exportation via crops/livestock (Leal et al, 2005;Vieira et al, 2015). Local depletion of forest regeneration sources, such as seeds, seedlings and resprouts can Caatinga soil 20.00 10 cm Tiessen et al, 1998 Caatinga soil 26.20 10 cm Kauffman et al, 1993 Caatinga soil 4.14 5 cm Schulz et al, 2016 Caatinga soil 17.00 5-60 cm Schulz et al, 2016 Caatinga soil 35.13-46.46 40 cm Barros et al, 2015 Caatinga slash and burn recovering soil 23.15 20 cm Althoff et al, 2018 Caatinga preserved soil 31.85 20 cm Althoff et al, 2018 Deserts and Semi Deserts soil 57.00 Across all horizons Prentice et al, 2001 Tropical Savannas and Grasslands soil 90.00 Across all horizons Prentice et al, 2001 Tropical Forest soil 122.00 Across all horizons Prentice et al, 2001 Temperate Forest soil 147.00 Across all horizons Prentice et al, 2001 Boreal Forest soil 274.00 Across all horizons Prentice et al, 2001 also be important (Tabarelli et al, 2017). Increased aridity (as predicted by climate change models; Torres et al, 2017) can magnify this human-induced degradation.…”
Section: Biocrusts As Ecosystem Service Providers and Their Role For mentioning
confidence: 99%