Specific Responses of Soil Microbial Residue Carbon to Long-Term Mineral Fertilizer Applications to Reddish Paddy Soils
References (46)
- et al.
Combining biomarker with stable isotope analyses for assessing the transformation and turnover of soil organic matter
Adv Agron
(2008) - et al.
Microbial colonisation of roots as a function of plant species
Soil Biol Biochem
(2006) - et al.
Relationships between microbial indices in roots and silt loam soils forming a gradient in soil organic matter
Soil Biol Biochem
(2006) - et al.
Comparison of factors limiting bacterial growth in different soils
Soil Biol Biochem
(2007) - et al.
Higher rates of manure application lead to greater accumulation of both fungal and bacterial residues in macroaggregates of a clay soil
Soil Biol Biochem
(2015) - et al.
Effects of tillage and crop rotation on soil microbial residues in a rainfed agroecosystem of northeast China
Soil Till Res
(2011) - et al.
Changes in soil microbial community composition in response to fertilization of paddy soils in subtropical China
Appl Soil Ecol
(2014) - et al.
Shifts in amino sugar and ergosterol contents after addition of sucrose and cellulose to soil
Soil Biol Biochem
(2007) - et al.
Amino sugars and muramic acid—biomarkers for soil microbial community structure analysis
Soil Biol Biochem
(2004) - et al.
Temporal responses of soil microorganisms to substrate addition as indicated by amino sugar differentiation
Soil Biol Biochem
(2011)
Effect of long-term fertilization on organic carbon and nitrogen in a subtropical paddy soil
Pedosphere
Quantitative assessment of the fungal contribution to microbial tissue in soil
Soil Biol Biochem
Microbial residues as indicators of soil restoration in South African secondary pastures
Soil Biol Biochem
Effects of long-term chemical fertilization and organic amendments on dynamics of soil organic C and total N in paddy soil derived from barren land in subtropical China
Soil Till Res
Preferential sequestration of microbial carbon in subsoils of a glacial-landscape toposequence, Dane County, WI, USA
Geoderma
Long-term effect of chemical fertilizer, straw, and manure on soil chemical and biological properties in northwest China
Geoderma
Effects of phosphorus addition on soil microbial biomass and community composition in three forest types in tropical China
Soil Biol Biochem
Microbial and soil properties in bentgrass putting greens: impacts of nitrogen fertilization rates
Geoderma
Effect of N and K fertilizers on yield and quality of greenhouse vegetable crops
Pedosphere
An assessment of the soil microbial status after 17 years of tillage and mineral P fertilization management
Appl Soil Ecol
Abundance, production and stabilization of microbial biomass under conventional and reduced tillage
Soil Biol Biochem
An extraction method for measuring soil microbial biomass C
Soil Biol Biochem
Carbon sequestration efficiency in paddy soil and upland soil under long-term fertilization in southern China
Soil Till Res
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The contribution of microbial necromass carbon to soil organic carbon in soil aggregates
2023, Applied Soil EcologyNitrogen slow-release behavior of oxamide granules in two different types of paddy soils
2022, PedosphereCitation Excerpt :Therefore, slower nitrification of NH4+ and reduced loss of NO3− through leaching and runoff were observed in the oxamide treatment than the urea treatment, similar to the results on polymer-coated urea treatments, leading to a small decrease amplitude of soil pH (Miah et al., 1998; 2000; Geng et al., 2015; Sun et al., 2019). Soil organic matter content increase in the N fertilizer treatments was attributed to greater root exudate and stubble and root residues due to better rice growth (Masto et al., 2006; Shen et al., 2007; Zhang et al., 2018). Since the stimulating effects of urea and oxamide on rice growth and yield were similar, there was little difference in the amplitude of the increase in soil organic matter between the urea and oxamide treatments.
The microbial-driven C dynamics within soil aggregates in walnut orchards of different ages based on microbial biomarkers analysis
2022, CatenaCitation Excerpt :The likely reason for these findings is that the higher living microbes in the larger aggregates could be beneficial for increasing microbial residues through its turnover (Murugan et al., 2019; Liang et al.,). For this purpose, the close connection between microbial residues and living microbes (as indicated by PLFAs) has been found in another study (Zhang et al., 2018), and in the present study as well (Fig. 6 and Fig. S2). The above-mentioned findings (i.e., the changes in microbial residues were caused by the variations of living microbes) were also the main reason for interpreting the changes in aggregate-associated microbial residues across walnut orchards of contrasting ages (Fig. 5).
Nitrogen addition increases microbial necromass in croplands and bacterial necromass in forests: A global meta-analysis
2022, Soil Biology and BiochemistryCitation Excerpt :Specifically, only the NPK addition, high N addition rate (>150 kg N ha−1 yr−1), and long-term N addition (>10 years) increased the contents of all individual and total amino sugars (Fig. 2a-d). For the positive effect of NPK addition on the contents of amino sugars, a possible explanation could be that increasing the availability of N, in combination with P and K, may have alleviated nutrient limitations on plant growth the most (Crowther et al., 2019) and therefore may have increased substrate availability the most (e.g., root exudates, litter input, TN and SOC content), thus favouring microbial growth and the production of microbial-derived components (Zhang et al., 2018b; Ye et al., 2019; Li et al., 2020; Ni et al., 2021). Furthermore, the response of amino sugars increased with increasing N addition rate (Figs. 4g, 6g and 7g), possibly because high N addition rates also increased substrate availability to microbes.
10-Year fertilization alters soil C dynamics as indicated by amino sugar differentiation and oxidizable organic C pools in a greenhouse vegetable field of Tianjin, China
2022, Applied Soil EcologyCitation Excerpt :The likely reasons for these findings are as follows. First, although MRC usually have longer turnover times in soils, it could be decomposed for the growth of plants and microbes in soils under no sufficient ORs inputs conditions (Liang et al., 2007; Zhang et al., 2018). Second, ORs (manure and/or straw) could provide sufficient C, which further promoted microbial growth and metabolism, and finally stored in the soils in the form of MRC (Fig. S4; Ding et al., 2013).
Contribution of soil microbial necromass to SOC stocks during vegetation recovery in a subtropical karst ecosystem
2021, Science of the Total Environment