2020
DOI: 10.5194/soil-6-523-2020
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Nitrogen availability determines the long-term impact of land use change on soil carbon stocks in grasslands of southern Ghana

Abstract: Abstract. Enhancing the capacity of agricultural soils to resist soil degradation and to mitigate climate change requires long-term assessments of land use systems. Such long-term evaluations, particularly regarding low-input livestock systems, are limited. In the absence of suitable long-term experiments, this study assessed the outcome of C inputs and outputs across an array of plant functional groups in arable and permanent systems of a tropical savannah after more than 50 years of consistent land use. Soil… Show more

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Cited by 9 publications
(8 citation statements)
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“…Similar results were obtained by Nguetnkam (2004) in the Far North Region of Cameroon and Moustakas (2012) in the north-eastern part of Greece. Low pH in the bleached layer of Planosols might be due to ferrolysis processes which have been suggested to explain oxides (Mn-Fe) segregation and gleying in such environments (Singh et al, 1998;Barbiero et al, 2010) and textural variations (O'Geen et al, 2008;Van Ranst et al, 2011;da Silva et al, 2019). It is common for Planosols to present pH < 5.5 due to acidification and destruction of clay minerals, leaving only quartz as the major constituent (Brinkman, 1970;Spiau and Pedro, 1986;Van Breemen and Buurman, 2002).…”
Section: Soil Physical Propertiesmentioning
confidence: 99%
See 1 more Smart Citation
“…Similar results were obtained by Nguetnkam (2004) in the Far North Region of Cameroon and Moustakas (2012) in the north-eastern part of Greece. Low pH in the bleached layer of Planosols might be due to ferrolysis processes which have been suggested to explain oxides (Mn-Fe) segregation and gleying in such environments (Singh et al, 1998;Barbiero et al, 2010) and textural variations (O'Geen et al, 2008;Van Ranst et al, 2011;da Silva et al, 2019). It is common for Planosols to present pH < 5.5 due to acidification and destruction of clay minerals, leaving only quartz as the major constituent (Brinkman, 1970;Spiau and Pedro, 1986;Van Breemen and Buurman, 2002).…”
Section: Soil Physical Propertiesmentioning
confidence: 99%
“…Studies on the Sudano-Sahelian part of the country are scare, and the few that exist are mainly available in unpublished reports or are more concerned with C stocks in plant biomass (Ibrahim and Habib, 2008;Tchobsala et al, 2014Tchobsala et al, , 2016. Moreover, many studies have ignored deeper SOC in the world (Ruiz Sinoda et al, 2012;Tornquist et al, 2009;Nyameasem et al, 2020;Schaefer et al, 2020;Mabicka et al, 2021). The present work aims to evaluate the SOC stock (SOCS) in the main soil types under the natural dry tropical area in the Sudano-Sahelian zone of Cameroon.…”
Section: Introductionmentioning
confidence: 99%
“…A possible reason explaining why the simulated soil nutrient dynamics may not properly capture the variability of nutrient balances observed across African savannas is because in the agro-ecosystems many cropping fields are selectively tilled with hoes, which is a less invasive technique than the broadcast tillage resulting from animal or mechanical traction plowing [119], as it is typically simulated in one-dimensional models. Finally, it must be pointed out that, despite significantly higher nutrient losses occur in the hydromorphic soil, regardless of the management treatment, this is likely to be driven by the higher levels of nutrient uptake by plants combined with biomass exported from the system, more than by the soil type itself.…”
Section: Nutrient Cycles and Nutrient Use Efficiencymentioning
confidence: 99%
“…The dataset, as well as a brief description of the site, materials and methods adopted to generate data is available in Nyameasem et al (2020).…”
Section: Plant Sampling and Proanthocyanidin Analysesmentioning
confidence: 99%