Abstract:Marginal land conversion to perennial energy crops can provide biomass feedstocks and climate change mitigation. However, the effect of perennial energy crop cultivation on soil organic carbon (SOC) sequestration and its underlying mechanism in marginal land still remains incomplete. Here, SOC turnover, stability, and its potential sequestration were evaluated based on 10 years of land use change from C3 grass‐dominated marginal land to C4 energy crops Miscanthus and switchgrass cultivation. The naturally occu… Show more
“…This was further supported by the positive correlation between four enzymes (i.e., BG, BX, CE, and ACP) and TN and NH 4 + and NO 3 − (Figure 4b). Concurrently, N can change the nutrient distribution ratio and indirectly affect soil enzyme activities (Xu et al, 2022). Also, soil pH influenced enzyme activities and enzymatic stoichiometry (Figure 4a).…”
Section: Discussionmentioning
confidence: 99%
“…The activities of soil enzymes, β‐1,4‐glucosidase (BG), β‐ D ‐xylopyranoside (BX), β‐ D ‐celliobiosidase (CE), β‐1,4‐ N ‐acetylglucosaminidas (NAG), L ‐leucine aminopeptidase (LAP), and acid phosphatase (ACP), were quantified with fluorogenically labelled substrates (Nayab et al, 2022; Xu et al, 2022; Zhou et al, 2021). In brief, add 50 mL distilled water to 1 g fresh soil, shake for 0.5 hr, and then aspirate 50 μL of the suspension.…”
Enhancing cropping intensity is the most effective and significant method to improve regional crop production and ensure food security. However, our understanding of the impacts of reduced cropping intensity on soil quality and ecosystem multifunctionality (EMF) with soil depth remains incomplete in tropical regions. Here, we performed a 4‐year field experiment to estimate the impacts of cropping intensity (continuous cropping, winter fallow, and annual fallow) on soil quality and EMF depending on soil depths. We found that reduced cropping intensity improved soil quality at the topsoil (0–10 cm), while it had no significant influences on soil carbon (C) and nitrogen (N) storage, as well as soil EMF at 0–40 cm. Soil microbes were limited by C and P but not co‐limited by N in all three cropping systems. Reduced cropping intensity exacerbated microbial C limitation at 0–10 cm due to reduced additional C resources (i.e., rice straw and manure) input. Redundancy analysis and Pearson correlation showed that soil N significantly affected the C‐, N‐, and P‐acquisition enzyme activities, and correlated positively with soil organic C, microbial biomass C, and available P. In conclusion, short‐term reduction in cropping intensity improves topsoil quality but not soil EMF under paddy‐upland rotations in the tropical region.
“…This was further supported by the positive correlation between four enzymes (i.e., BG, BX, CE, and ACP) and TN and NH 4 + and NO 3 − (Figure 4b). Concurrently, N can change the nutrient distribution ratio and indirectly affect soil enzyme activities (Xu et al, 2022). Also, soil pH influenced enzyme activities and enzymatic stoichiometry (Figure 4a).…”
Section: Discussionmentioning
confidence: 99%
“…The activities of soil enzymes, β‐1,4‐glucosidase (BG), β‐ D ‐xylopyranoside (BX), β‐ D ‐celliobiosidase (CE), β‐1,4‐ N ‐acetylglucosaminidas (NAG), L ‐leucine aminopeptidase (LAP), and acid phosphatase (ACP), were quantified with fluorogenically labelled substrates (Nayab et al, 2022; Xu et al, 2022; Zhou et al, 2021). In brief, add 50 mL distilled water to 1 g fresh soil, shake for 0.5 hr, and then aspirate 50 μL of the suspension.…”
Enhancing cropping intensity is the most effective and significant method to improve regional crop production and ensure food security. However, our understanding of the impacts of reduced cropping intensity on soil quality and ecosystem multifunctionality (EMF) with soil depth remains incomplete in tropical regions. Here, we performed a 4‐year field experiment to estimate the impacts of cropping intensity (continuous cropping, winter fallow, and annual fallow) on soil quality and EMF depending on soil depths. We found that reduced cropping intensity improved soil quality at the topsoil (0–10 cm), while it had no significant influences on soil carbon (C) and nitrogen (N) storage, as well as soil EMF at 0–40 cm. Soil microbes were limited by C and P but not co‐limited by N in all three cropping systems. Reduced cropping intensity exacerbated microbial C limitation at 0–10 cm due to reduced additional C resources (i.e., rice straw and manure) input. Redundancy analysis and Pearson correlation showed that soil N significantly affected the C‐, N‐, and P‐acquisition enzyme activities, and correlated positively with soil organic C, microbial biomass C, and available P. In conclusion, short‐term reduction in cropping intensity improves topsoil quality but not soil EMF under paddy‐upland rotations in the tropical region.
“…These plants are considered perennial energy, whose root systems efficiently sequester SOC through a rapid rate of renovation of the SOC. In other words, the new C4-derived C replaced the old C3-C at a rate sufficient to offset the losses (Xu et al, 2022). The SOM content derived from C4 cultures has a faster decomposition than C3.…”
Land‐use change has driven soil carbon stock losses in ecosystems worldwide. Implementing agricultural crops and exploiting forest resources trigger the breakdown of soil aggregates, thus exposing organic matter to microbial decomposition and enhancing carbon dioxide emissions, especially in biomes more susceptible to climate extremes as in the tropical semiarid regions. This study was based on the hypothesis that the undisturbed soil from the dry forest (Caatinga biome under natural revegetation in Brazilian semiarid) would have an improvement in the mass of macroaggregates and recover more than 50% of the soil C stock within 10 years. Thus, a field experiment was conducted to investigate soils from the Caatinga biome under native vegetation, “cowpea cropping” for over 30 years, and soil under natural revegetation for over 10 years, after conventional soil cultivation of maize and cowpea, to determine soil and soil‐aggregates carbon stocks and to estimate the recovery rate of these stocks. The proportional mass of aggregates of different sizes and the total stock of particulate organic carbon (POC) were also quantified. The results showed that soil under preserved native vegetation of dry forest Caatinga biome had higher total soil C stock (50.9 Mg ha−1) than that under cowpea cropping (23.2 Mg ha−1) and natural revegetation (45.1 Mg ha−1). The proportional mass of large macroaggregates was higher in soil under native vegetation for all depths. However, soil under cowpea cropping had lower C stocks in macroaggregates, and recovered roughly 63% of the original C stocks, while revegetation recovered 78% of the stock in 10 years. Although the conventional management system for cowpea monoculture aggravated losses in soil carbon stock by more than 50% of the original C stocks, dry forest under natural revegetation recovered 79% of this stock and almost 100% of POC stock in 10 years (~12 Mg ha−1). Furthermore, soil under undisturbed Caatinga dry forest achieved C stock levels equivalent to that of the global average range for semiarid tropical environments. The high recovery rate of C stock in forest soil under natural revegetation indicates the resilience potential of organisms responsible for structural protection of aggregates and the encapsulated soil organic matter content.
“…Controlled release N fertilizer has advantages with respect to maintaining and increasing leaf greenness as a result of providing continuous N supplement, which indirectly increases carbon dioxide assimilation for the remobilization of non‐structural carbohydrates to grain organs 5,15 . Both controlled and field experiments suggest that supplementation with controlled release N fertilizer increases cereal crop morphology traits, gas exchange attributes, and soil inorganic N and organic C content over the reproductive period 16‐18 . Short‐term straw returning fertilization effects on crop yields are likely to reduce because of the uncertainty in the quality and quantality of straw decomposition to nutrients over the changing growing season 19,20 …”
Section: Introductionmentioning
confidence: 99%
“…5,15 Both controlled and field experiments suggest that supplementation with controlled release N fertilizer increases cereal crop morphology traits, gas exchange attributes, and soil inorganic N and organic C content over the reproductive period. [16][17][18] Short-term straw returning fertilization effects on crop yields are likely to reduce because of the uncertainty in the quality and quantality of straw decomposition to nutrients over the changing growing season. 19,20 Conventional N urea application practices (such as multiple application and subsurface placement) enhance leaf development, N allocation to harvest organs and decrease the N losses to environment.…”
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