Silicon fertilizer and biochar effects on plant and soil PhytOC concentration and soil PhytOC stability and fractionation in subtropical bamboo plantations

2021 ◽  
Author(s):  
Chengpeng Huang ◽  
Li Wang ◽  
Xiaoqiang Gong ◽  
Zhangting Huang ◽  
Miaorong Zhou ◽  
...  
Keyword(s):  
Fertilizer Application ◽  
Moso Bamboo ◽  
Pool Size ◽  
Phyllostachys Pubescens ◽  
Soil System ◽  
Organic C ◽  
Soil Organic Nitrogen ◽  
Plant Soil ◽  
Application Rates ◽  
The Impact

<p>The use of exogenous silicon (Si) amendments, such as Si fertilizers and biochar, can effectively increase crop Si uptake and the formation of phytoliths, which are siliceous substances that are abundant in numerous plant species. Phytolith-occluded carbon (C) (PhytOC) accumulation in soil plays an important role in long-term soil organic C (SOC) storage. Nevertheless, the effects of both Si fertilizer and biochar application on PhytOC sequestration in forest plant-soil systems have not been studied. We investigated the impact of Si fertilizer and biochar applications on 1) the PhytOC pool size, the solubility of plant and soil phytoliths, and soil PhytOC in soil physical fractions (light (LFOM) and heavy fractions of organic matter (HFOM)) in Moso bamboo (<em>Phyllostachys pubescens</em>) forests; and 2) the relationships among plant and soil PhytOC concentrations and soil properties. We used a factorial design with three Si fertilizer application rates: 0 (S0), 225 (S1) and 450 (S2) kg Si ha<sup>−1</sup>, and two biochar application rates: 0 (B0) and 10 (B1) t ha<sup>−1</sup>. The concentrations of PhytOC in the bamboo plants and topsoil (0–10 cm) increased with increasing Si fertilizer addition, regardless of biochar application. Biochar addition increased the soil PhytOC pool size, as well as the LFOM- and HFOM-PhytOC fractions, regardless of Si fertilizer application. The Si fertilizer application increased or had no effect on soil phytolith solubility with or without biochar application, respectively. Soil PhytOC was correlated with the concentration of soil organic nitrogen (R<sup>2</sup>=0.32), SOC (R<sup>2</sup>=0.51), pH (R<sup>2</sup>=0.28), and available Si (R<sup>2</sup>=0.23). Furthermore, Si fertilizer application increased plant and soil PhytOC by increasing soil available Si. Moreover, biochar application increased soil PhytOC concentration in LFOM-PhytOC and the unstable fraction of PhytOC. We conclude that Si fertilizer and biochar application promoted PhytOC sequestration in the plant-soil system and changed its distribution in physical fractions in the Moso bamboo plantation in subtropical China.</p>

scholarly journals Biochar-based organic fertilizer application rates for Tetrastigma hemsleyanum planted under Moso bamboo

2019 ◽  
Vol 31 (5) ◽  
pp. 1813-1821 ◽  
Author(s):  
Xiaoping Zhang ◽  
Guibin Gao ◽  
Zhizhuang Wu ◽  
Xing Wen ◽  
Fangyuan Bian ◽  
...  
Keyword(s):  
Organic Fertilizer ◽  
Fertilizer Application ◽  
Moso Bamboo ◽  
Tetrastigma Hemsleyanum ◽  
Application Rates

scholarly journals Quantifying N2O emissions from intensive grassland production: the role of synthetic fertilizer type, application rate, timing and nitrification inhibitors

2016 ◽  
Vol 154 (5) ◽  
pp. 812-827 ◽  
Author(s):  
M. J. BELL ◽  
J. M. CLOY ◽  
C. F. E. TOPP ◽  
B. C. BALL ◽  
A. BAGNALL ◽  
...  
Keyword(s):  
Nitrous Oxide ◽  
Fertilizer Application ◽  
Application Rate ◽  
Nitrous Oxide Emissions ◽  
Mineral Fertilizers ◽  
Urea Fertilizer ◽  
Mitigation Options ◽  
Application Rates ◽  
The Impact ◽  
Ipcc Default

SUMMARYIncreasing recognition of the extent to which nitrous oxide (N2O) contributes to climate change has resulted in greater demand to improve quantification of N2O emissions, identify emission sources and suggest mitigation options. Agriculture is by far the largest source and grasslands, occupying c. 0·22 of European agricultural land, are a major land-use within this sector. The application of mineral fertilizers to optimize pasture yields is a major source of N2O and with increasing pressure to increase agricultural productivity, options to quantify and reduce emissions whilst maintaining sufficient grassland for a given intensity of production are required. Identification of the source and extent of emissions will help to improve reporting in national inventories, with the most common approach using the IPCC emission factor (EF) default, where 0·01 of added nitrogen fertilizer is assumed to be emitted directly as N2O. The current experiment aimed to establish the suitability of applying this EF to fertilized Scottish grasslands and to identify variation in the EF depending on the application rate of ammonium nitrate (AN). Mitigation options to reduce N2O emissions were also investigated, including the use of urea fertilizer in place of AN, addition of a nitrification inhibitor dicyandiamide (DCD) and application of AN in smaller, more frequent doses. Nitrous oxide emissions were measured from a cut grassland in south-west Scotland from March 2011 to March 2012. Grass yield was also measured to establish the impact of mitigation options on grass production, along with soil and environmental variables to improve understanding of the controls on N2O emissions. A monotonic increase in annual cumulative N2O emissions was observed with increasing AN application rate. Emission factors ranging from 1·06–1·34% were measured for AN application rates between 80 and 320 kg N/ha, with a mean of 1·19%. A lack of any significant difference between these EFs indicates that use of a uniform EF is suitable over these application rates. The mean EF of 1·19% exceeds the IPCC default 1%, suggesting that use of the default value may underestimate emissions of AN-fertilizer-induced N2O loss from Scottish grasslands. The increase in emissions beyond an application rate of 320 kg N/ha produced an EF of 1·74%, significantly different to that from lower application rates and much greater than the 1% default. An EF of 0·89% for urea fertilizer and 0·59% for urea with DCD suggests that N2O quantification using the IPCC default EF will overestimate emissions for grasslands where these fertilizers are applied. Large rainfall shortly after fertilizer application appears to be the main trigger for N2O emissions, thus applicability of the 1% EF could vary and depend on the weather conditions at the time of fertilizer application.

IMPACT OF ELEMENTAL SULFUR FERTILIZATION ON AGRICULTURAL SOILS. I. EFFECTS ON MICROBIAL BIOMASS AND ENZYME ACTIVITIES

1988 ◽  
Vol 68 (3) ◽  
pp. 463-473 ◽  
Author(s):  
V. V. S. R. GUPTA ◽  
J. R. LAWRENCE ◽  
J. J. GERMIDA
Keyword(s):  
Microbial Biomass ◽  
Elemental Sulfur ◽  
Agricultural Soils ◽  
Microbial Biomass Carbon ◽  
Fertilizer Application ◽  
Biomass Carbon ◽  
Repeated Application ◽  
Organic C ◽  
The Impact ◽  
Sulfur Fertilization

This study investigated the impact of repeated application of S° fertilizer on microbial and biochemical characteristics of two Grey Luvisolic soils. The Waitville pasture plots received Agri-Sul at a rate of 22 or 44 kg S° ha−1 yr−1 for 5 yr, whereas the Loon River canola-summerfallow plots received single or double applications of Flow-able Sulfur (50 kg S° ha−1) or Agri-Sul (100 kg S° ha−1). Application of S° fertilizer significantly decreased the pH in both soils. Organic C declined in S°-treated plots of the Waitville soil, and there was a narrowing of C:N:S ratios in both soils. Application of S° fertilizer significantly increased the total S, HI-S and sulfate sulfur levels of both soils. There was a 29–45% and 2–51% decline in microbial biomass carbon content due to S° fertilizer application in Waitville and Loon River soils, respectively. Repeated application of S° also resulted in a decline in respiration, dehydrogenase, urease, alkaline phosphatase and arylsulfatase activities, along with populations of protozoa, algae and nitrifiers in both soils. Significant correlations observed among related characteristics further emphasized the treatment effects. These results indicate that the impact of repeated application of S° fertilizer on microbial biomass and activity should be considered when recommending S° as a fertilizer for sulfur-deficient soils. Key words: Sulfur (elemental), microbial biomass, dehydrogenase, urea, phosphomonoesterases, arylsulfatase

scholarly journals Changing Fertilizer Management Practices in Sugarcane Production: Cane Grower Survey Insights

2020 ◽  
Author(s):  
Syezlin Hasan ◽  
James C. R. Smart ◽  
Rachel Hay ◽  
Sharyn Rundle-Thiele
Keyword(s):  
Management Practices ◽  
Negative Binomial ◽  
Fertilizer Application ◽  
Application Rate ◽  
Practice Change ◽  
Farm Income ◽  
Fertilizer Management ◽  
Application Rates ◽  
Fertilizer Application Rate ◽  
The Impact

Research focused on understanding wider systemic factors driving behavioral change is limited with a dominant focus on the role of individual farmer and psychosocial factors for farming practice change, including reducing fertilizer application in agriculture. Adopting a wider systems perspective, the current study examines change and the role that supporting services have on fertilizer application rate change. A total of 238 sugarcane growers completed surveys reporting on changes in fertilizer application along with factors that may explain behavior change. Logistic regressions and negative binomial count-data regressions were used to examine whether farmers had changed fertilizer application rates and if they had, how long ago they made the change, and to explore the impact of individual and system factors in influencing change. Approximately one in three sugarcane growers surveyed (37%) had changed the method they used to calculate fertilizer application rates for the cane land they owned/managed at some point. Logistic regression results indicated growers were less likely to change the basis for their fertilizer calculation if they regarded maintaining good relationships with other local growers as being extremely important, they had another source of off-farm income, and if they had not attended a government-funded fertilizer management workshop in the five years preceding the survey. Similar drivers promoted early adoption of fertilizer practice change; namely, regarding family traditions and heritage as being unimportant, having sole decision-making authority on farming activities and having attended up to 5 workshops in the five years prior to completing the survey. Results demonstrated the influence of government-funded services to support practice change.

The impact of relative humidity, genotypes and fertilizer application rates on panicle, leaf temperature, fertility and seed setting of rice

2010 ◽  
Vol 148 (3) ◽  
pp. 329-339 ◽  
Author(s):  
C. YAN ◽  
Y. DING ◽  
Q. WANG ◽  
Z. LIU ◽  
G. LI ◽  
...  
Keyword(s):  
Relative Humidity ◽  
Air Temperature ◽  
Flag Leaf ◽  
Canopy Temperature ◽  
Fertilizer Application ◽  
Spikelet Fertility ◽  
Nitrogen Application ◽  
Seed Setting ◽  
Application Rates ◽  
The Impact

SUMMARYA series of field and plant growth chamber experiments were conducted in 2006 and 2007 to study how relative humidity (RH), genotypes and nitrogen application rates affect organ temperatures and spikelet fertility rates in rice. It was observed that organ temperatures varied with air temperature, RH, genotype and nitrogen application rate. Increases in RH at constant air temperature and increasing air temperature with a constant RH both increased organ temperatures significantly. Cultivars also exhibited differences in organ temperatures; those cultivars with erect panicles recorded lower organ temperatures than those with droopy panicles under similar climatic conditions. Similarly, cultivars with panicles above the flag leaf had lower temperatures at the panicle when compared to those plants with the panicle below the flag leaf. It was also found that panicle temperature showed a significant negative correlation with both grain filling rate and seed setting rate. Spikelet fertility could be maintained by reducing spikelet temperature under decreasing RH in a high-temperature environment. Panicle fertilizer application rates had a significant effect on the organ and canopy temperatures. The canopy temperature of rice grown with an ample supply of nitrogen was generally cooler than the canopy temperature of a nitrogen-deficient treatment.

Pastures and drought: a review of processes and implications for nitrogen and phosphorus cycling in grassland systems

Soil Research ◽  
2019 ◽  
Vol 57 (2) ◽  
pp. 101 ◽  
Author(s):  
Gina M. Lucci
Keyword(s):  
Soil Microorganisms ◽  
Future Climate Change ◽  
Nitrogen And Phosphorus ◽  
Soil System ◽  
Plant Soil ◽  
Community Population ◽  
Stocks And Flows ◽  
Effects Of Drought ◽  
The Impact ◽  
Cycling Of Nutrients

The incidence and extent of drought is predicted to increase and therefore understanding the effects on the plant–soil system is important. The objective of this review is to report on the fundamental processes involved in the effects of drought on pasture, soil, and soil microorganisms in grassland systems and evaluate the consequences of drought to determine whether management decisions could mitigate the impact of drought. There are associations within the plant–soil system affecting the flows and cycling of nutrients. Drought conditions often create a flush of nitrogen, carbon, and phosphorus upon rewetting that is at risk of loss to the environment. Prediction of the flush magnitude is difficult because it is influenced by drought characteristics such as duration, soil temperature, degree of drying, and rate at which the rewetting occurs post-drought. Response to drought is also affected by the microbial community population and structure of the soil-related flora and fauna. Increasing pasture diversity and soil organic matter may help to mitigate the effects of drought in grassland systems. More research is needed that incorporates all the components of the plant–soil system to examine the net effects of drought on grassland systems. Better measures are also needed to estimate the consequences for future climate change on nutrient stocks and flows.

scholarly journals Black Soldier Fly Diet Impacts Soil Greenhouse Gas Emissions From Frass Applied as Fertilizer

2021 ◽  
Vol 5 ◽  
Author(s):  
Pauline Sophie Rummel ◽  
Lukas Beule ◽  
Michael Hemkemeyer ◽  
Sanja Annabell Schwalb ◽  
Florian Wichern
Keyword(s):  
Greenhouse Gas ◽  
Ghg Emissions ◽  
Strong Increase ◽  
Functional Genes ◽  
Ammonia Oxidizing Bacteria ◽  
Black Soldier Fly ◽  
Organic C ◽  
Application Rates ◽  
C And N ◽  
The Impact

Increased global production of animal-based protein results in high greenhouse gas (GHG) emissions and other adverse consequences for human and planetary health. Recently, commercial insect rearing has been claimed a more sustainable source of animal protein. However, this system also leaves residues called frass, which—depending on the insect diet—is rich in carbon (C) and nitrogen (N), and could thus be used as fertilizer in agriculture. The impact of this kind of fertilizer on soil GHG emissions is yet unknown. Therefore, we investigated the effect of black soldier fly (Hermetia illucens L.) frass derived from a carbohydrate (Carb-) or a protein (Prot-) based diet applied at two different application rates to an arable soil on C and N fluxes and microbial properties in a 40-day incubation experiment. CO2, N2O, NO, N2, CH4, water extractable organic C (WEOC), and inorganic N were continuously measured quantitatively. At the end of the incubation, microbial biomass (MB), stoichiometry, community composition, and abundance of functional genes were assessed. Along with a strong increase in WEOC and CO2, Carb-frass caused strong initial N2O emissions associated with high N and C availability. In contrast, Prot-frass showed lower CO2 emissions and N2O release, although soil nitrate levels were higher. At the end of incubation, MB was significantly increased, which was more pronounced following Carb-frass as compared to Prot-frass application, and at higher amendment rates. Fungal abundance increased most from both frass types with an even stronger response at higher application rates, whereas bacterial abundance rose following Carb-frass as compared to Prot-application. Abundance of functional genes related to ammonia-oxidizing bacteria and archaea were enhanced by high frass application but did not clearly differ between frass types. C use efficiency of microorganisms, as revealed by the metabolic quotient, was most strongly reduced in the high Prot-frass application rate. Overall, insect diet influenced available C and N in frass and thus affected mineralization dynamics, GHG emissions, and microbial growth. Overall, emissions were very high undermining the potential environmental benefit of insect based protein production and calling for more detailed analyses before frass is widely applied in agriculture.

Temporal evolution of C stock in soils from the cork oak forest in a post-fire scenario

2021 ◽  
Author(s):  
Patricia Almeida ◽  
Erika S. Santos ◽  
Diego Arán ◽  
Vanda Acácio ◽  
Inês Duarte ◽  
...  
Keyword(s):  
Temporal Evolution ◽  
Cork Oak ◽  
Tree Level ◽  
Oak Forest ◽  
Soil System ◽  
Organic C ◽  
C Stock ◽  
Cork Oak Forest ◽  
Burnt Areas ◽  
The Impact

<p>Forest fires are increasing their recurrence, intensity and scale in Portugal, increasing also the vulnerability of this region of Southwestern Europe to the impacts of the climate change. In Portugal, several studies have been focusing the dynamic of cork oak forest after fires from tree level to landscape level. However few information is available about the impact of wildfires in the soil quality, namely C stock, and its evolution. This component of the ecosystem and the evolution of its characteristics can be related with the dynamics of the landscape in the post-fire period and its knowledge can help in the management and rehabilitation of plant-soil system.</p><p>Serra do Caldeirão is located in Algarve region (S of Portugal). The soils are classified as Leptosols with low fertility. The landscape is characterized by cork oak forests with shrub cover which is dominated by Cistus species. To assess the distribution of total organic C in the study area, several soil sampling were intersected, on two sampling dates (2012 and 2013), with the vector information of the burned area in 2004. This information was intended to assess the temporal evolution of C concentration, depending on its location in a burnt or non-burnt area.</p><p>In general, the burnt areas showed greater variability of C concentrations in soils collected in both the years, with maximum values ​​of 33.0 g/kg for 2012 and 36.5 g/kg for 2013. These maximum values ​​exceed those obtained for soils in non-burnt areas. Despite of this scenario, and independently of the year, no statistically significant differences were found in the C concentrations of the burnt plots and the control plots. For other chemical characteristics (e.g. nutrients), the variations depended on the area. Implementation of post-fire recovery measures and forest management of the areas can justify this variation.</p><p>Acknowledgment: This work is co-financed by project REMAS (SOE3/P4/E0954) from Interreg SUDOE 2014-2020 program and is also financed by the FEDER Funds through the Operational Competitiveness Factors Program - COMPETE and by National Funds through FCT - Foundation for Science and Technology within the scope of the project  UID/AGR/04129/2020 (LEAF) and  the project UID/BIA/50027/2019 (CEABN/InBIO).</p>

Considerations for the mitigation of nitrate contamination: stable isotopes and insights into the importance of soil processes

2011 ◽  
Vol 64 (6) ◽  
pp. 1254-1260 ◽  
Author(s):  
George H. Somers ◽  
Martine M. Savard
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Nutrient Management ◽  
Growing Season ◽  
Fertilizer Application ◽  
Nitrate Contamination ◽  
N Application ◽  
Application Rates ◽  
Direct Leaching ◽  
The Impact

Nutrient management is widely promoted to minimize the impact of intensive fertilizer use on groundwater quality, however watershed-scale stable isotope studies in eastern North America suggest nitrogen transport to groundwater is dominated by non-growing season fluxes derived principally from the mineralization and nitrification of soil organic matter. In the current field scale study, δ15N ratios of nitrate in tile drain effluents from experimental potato plots treated with 300 kg/ha ammonia nitrate and those with no fertilizer both average +4.7‰, close to the +4.0‰ ratios observed in soils of the same plots, and distinct from values near 0‰ for inorganic fertilizer. A source apportionment model using δ15N and δ18O in nitrate suggests that even with heavy fertilizer application, less than 10% of non-growing season N flux is derived from direct leaching of fertilizer, the remainder representing N from various sources, including residual fertilizer that has been assimilated into the broader soil organic matter pool and subsequently released via mineralization and nitrification. Factors controlling these losses could be as closely related to cropping practices as initial N application rates, providing potential opportunities for more efficiently utilizing N available in the soil profile and reducing initial N application rates.

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