C and N mineralization in sandy and loamy grassland soils: The role of microbes and microfauna
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Soil organic carbon in sandy soils: A review
2019, Advances in AgronomySoil texture and phosphorous under two contrasting land use types in the Loess Plateau
2019, CatenaCitation Excerpt :We observed significant increases in the contents of OC and N in bulk soils and increases in the P contents in macro- and microaggregates with clay content (Fig. 3). The increasing relationships of OC and N in bulk soils with clay content have been reported in various ecosystems (Hassink and Neutel, 1994; Galantini et al., 2004; Gami et al., 2009; Adhikari and Bhattacharyya, 2015) and have been ascribed to the accumulation of OC and N in clay particles due to the chemical association with mineral surfaces (Lützow et al., 2006; Grüneberg et al., 2013). However, the effects of soil texture on aggregates associated with OC, N and P have been less examined, particularly in various land use conditions.
Stoichiometric linkages between plant litter, trophic interactions and nitrogen mineralization across the litter-soil interface
2016, Soil Biology and BiochemistryCitation Excerpt :Organism-oriented models, which explicitly incorporate soil organisms and their interactions with the biophysical environment, have a high explanatory value and permit the evaluation of the effects of intervention and management (Paustian, 1994; Smith et al., 1998). The quantitative food-web modeling approach initiated by Hunt et al. (1987) has been applied to several natural and agricultural systems and has proven useful in simulating C and N mineralization rates and in explaining rates in terms of the relative contribution of groups of organisms and particular trophic interactions (Hassink et al., 1994; de Ruiter et al., 1994; Berg et al., 2001; Schroter et al., 2003; Bezemer et al., 2010). In this approach food webs are constructed by aggregating species into functional groups and N and C cycling are analyzed in relation to the structure and functioning of the food webs.
Modification of maize simulation model for predicting growth and yield of winter wheat under different applied water and nitrogen
2015, Agricultural Water ManagementCitation Excerpt :The average value of mineralized N in the soil was 18 kg N ha−1 in 2010–2011. Hassink et al. (1994) reported the value of 65 kg N ha−1 year−1 for the mineralization rate in a loamy soil with 1.77% and 0.15% of organic C and organic N, respectively. Due to the low value of organic matter of the experimental field (Table.
Effects of sieving, drying and rewetting upon soil bacterial community structure and respiration rates
2010, Journal of Microbiological MethodsCitation Excerpt :The lack of studies utilising molecular techniques is surprising as these are now commonly used tools in soil microbial ecology. Bacteria are the most abundant soil microbes and, as a result, are intrinsic to soil functioning (Beare et al., 1995; Hassink et al., 1994). Therefore, our aim was to investigate the effects of soil homogenisation techniques on bacterial community structure and respiration rates, by comparing intact soil cores with freshly sieved soil and soil which had been sieved, dried and rewetted.
Modeling field-scale N mineralization in Coastal Plain soils (USA)
2007, Ecological Modelling