2011
DOI: 10.1016/j.soilbio.2010.12.012
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Microbial residues as indicators of soil restoration in South African secondary pastures

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Cited by 64 publications
(19 citation statements)
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“…Several other studies conducted under similar and different climates and soil conditions (Bach et al, 2010; Preger et al, 2010; Lauer et al, 2011; Kösters et al, 2013; Baer et al, 2015; Wang et al, 2016; Kiani et al, 2017) conform with our results that revealed possible reversal of historic SOC and SIC after croplands were reverted to perennial pastures (Fig. 2).…”
Section: Discussionsupporting
confidence: 91%
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“…Several other studies conducted under similar and different climates and soil conditions (Bach et al, 2010; Preger et al, 2010; Lauer et al, 2011; Kösters et al, 2013; Baer et al, 2015; Wang et al, 2016; Kiani et al, 2017) conform with our results that revealed possible reversal of historic SOC and SIC after croplands were reverted to perennial pastures (Fig. 2).…”
Section: Discussionsupporting
confidence: 91%
“…Exclusion of intensive cultivation in the secondary grasslands reduced SOC decomposition rates and stabilized SIC dissolution‐precipitation processes (Wang et al, 2016; Kiani et al, 2017; Li et al, 2018). Minimum decomposition under secondary grassland management is a benefit in sandy soils with low C protective capacity (Preger et al, 2010; Lauer et al, 2011; Kösters et al, 2013).…”
Section: Discussionmentioning
confidence: 99%
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“…The ratio of soil carbon to nitrogen was 5.39 in cropland and 5.85 in grassland, and the ratio of root carbon to nitrogen was 38 in cropland and 61 in grassland, respectively. There were more fungi in grassland than in cropland (Lauer et al, 2011), and the biochemically recalcitrant substrates would be more depleted in this case (Djukic et al, 2010). Q 10 was larger in relatively labile substrates than in biochemically recalcitrant substrates (Guntinas et al, 2013).…”
Section: Land-use Conversions Influenced Temperature Sensitivity Of Smentioning
confidence: 90%
“…We found distinct responses of physical, physicochemical, and biological indicators to grazing management. Soils in the focal SES's piospheres were highly degraded, indicated by soil compaction attributable to animal trampling, aggregate disruption, and associated decomposition of soil organic carbon, and a decoupling of biological soil processes (Lauer et al 2011). Physico-chemical and biological degradation were most likely caused by low litter production due to the removal of biomass (Angassa et al 2012).…”
Section: Soil Resiliencementioning
confidence: 99%