2017
DOI: 10.1016/j.biombioe.2017.07.023
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Carbon stocks in necromass and soil pools of a Mozambican tropical dry forest under different disturbance regimes

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Cited by 11 publications
(10 citation statements)
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“…Moreover, the SOC and TN stocks in the MW sites in the study area are also lower than estimations of 34.09 Mg ha -1 of SOC and 6.75 Mg ha -1 of TN found in Zambian MW (Mlambo et al 2007). Furthermore, our findings contrast with those of other studies, which reported higher SOC stocks in AF (Molotja et al 2011;Khavhagali and Ligavha-Mbelengwa 2009;Magalhães 2017). The lower SOC and TN stock observed in this study can be attributed to several factors such as low productivity under variable moisture and temperature, erratic rainfall and low soil water-holding capacities at the study site (Evan and Ehleringer 1994;Scholes and Archer 1997;Lal 2014).…”
Section: Relationship Between Woodland Type and Soil Organic Carbon Acontrasting
confidence: 94%
“…Moreover, the SOC and TN stocks in the MW sites in the study area are also lower than estimations of 34.09 Mg ha -1 of SOC and 6.75 Mg ha -1 of TN found in Zambian MW (Mlambo et al 2007). Furthermore, our findings contrast with those of other studies, which reported higher SOC stocks in AF (Molotja et al 2011;Khavhagali and Ligavha-Mbelengwa 2009;Magalhães 2017). The lower SOC and TN stock observed in this study can be attributed to several factors such as low productivity under variable moisture and temperature, erratic rainfall and low soil water-holding capacities at the study site (Evan and Ehleringer 1994;Scholes and Archer 1997;Lal 2014).…”
Section: Relationship Between Woodland Type and Soil Organic Carbon Acontrasting
confidence: 94%
“…The region has pedogeomorphologic gradients with aluminum-rich dystrophic latosols at the tops of hills, colluvial ramps with shallow latosols and cambic horizon, while the bottoms of the groves present a predominance of epieutrophic cambisols rich in nutrients [24]. for invertebrates and vertebrates [13], integration of forest nutrient cycling [14,15], and storing carbon [16][17][18]. Necromass is estimated to be responsible for stocking 73.0 ± 6.0 PgC, representing 8% of the world's forest carbon [19].…”
Section: Description Of the Study Areamentioning
confidence: 99%
“…This increase in tree mortality leads to a greater accumulation of necromass (dead organic matter) that can remain on tropical forest soil for more than 30 years [10]. Necromass plays a key role during this phase of the forest ecosystem, providing food for saproxylic organisms [11,12], habitat for invertebrates and vertebrates [13], integration of forest nutrient cycling [14,15], and storing carbon [16][17][18].…”
Section: Introductionmentioning
confidence: 99%
“…A homogenized subsample of the soil (disturbed soil sample) was collected at each soil depth and kept in an airtight polythene bag. The soil pits were cleared vertically and two soil cores (undisturbed soil samples) taken horizontally, at two vertical positions along the soil pit, one at each half of each soil depth, using a 100 cm 3 volume corer (height: 51 mm, inner diameter: 50 mm) (Magalhães, 2017; Magalhães & Mamugy, 2020).…”
Section: Methodsmentioning
confidence: 99%