Antimony mobility in Japanese agricultural soils and the factors affecting antimony sorption behavior

2006 ◽  
Vol 141 (2) ◽  
pp. 321-326 ◽  
Author(s):  
Yasuo Nakamaru ◽  
Keiko Tagami ◽  
Shigeo Uchida
2020 ◽  
Author(s):  
Laura Heimsch ◽  
Annalea Lohila ◽  
Liisa Kulmala ◽  
Juha-Pekka Tuovinen ◽  
Mika Korkiakoski ◽  
...  

<p>Agriculture is globally a significant source of carbon emissions to the atmosphere. Main causes for these high emissions are conventional intensive management practices which include such as frequent ploughing, monocropping and high use of agrochemicals. These practices contribute to the loss of biodiversity and soil organic matter, as well as to the CO<sub>2</sub> emissions from land use. Recently, it has been recognised that agriculture functioning on the basis of regenerative practices is one of the most potential tools to mitigate climate change.</p><p>It is well known that topsoil layer and especially humus-rich soils can store more carbon than atmosphere and vegetation together. Therefore, increasing the amount of soil organic matter in the agroecosystems, by applying enhanced management practices such as reduced tillage, high biodiversity and cover cropping, agricultural soils would not only help to mitigate climate change but also to restore soil quality and fertility. To understand the carbon dynamics on different agricultural sites, factors affecting and comprising the carbon balance, and to verify soil carbon and ecosystem models, continuous long-term monitoring of the GHG fluxes is essential at such managed ecosystems. Here we present results from a new eddy covariance (EC) flux study site located in southern Finland.</p><p>Continuous CO<sub>2</sub> flux measurements using the EC method have been conducted at Qvidja farm on mineral (clay) soil forage grassland in Parainen, southern Finland (60.29550°N, 22.39281°E) since the spring 2018. Based on the flux and biomass data, the annual carbon balance was estimated to be negative, i.e. the site acted as an overall sink of carbon even in the dry and hot year 2018. However, the seasonal CO<sub>2</sub> fluxes were greatly dependent on weather conditions and management procedures. Results from 2019 show that the growing season accompanied with more mature and dense grass, a bit higher precipitation and lower temperatures, as well as higher cutting height was more favorable for carbon uptake in Qvidja as compared to year 2018.</p>


2001 ◽  
Vol 32 (17-18) ◽  
pp. 2679-2690 ◽  
Author(s):  
M. E. Conti ◽  
A. M. de la Horra ◽  
D. Effron ◽  
D. Zourarakis

Author(s):  
Sascha Setzer ◽  
Dorit Julich ◽  
Stefan Gäth

2016 ◽  
Vol 89 (6) ◽  
pp. 988-999 ◽  
Author(s):  
H. M. H. Gad ◽  
H. A. Elsanafini ◽  
M. M. S. Ali ◽  
Y. F. Lasheen ◽  
M. G. Abdelwahed

2007 ◽  
Vol 97 (2) ◽  
pp. 250-256 ◽  
Author(s):  
David M. Weller

Pseudomonas spp. are ubiquitous bacteria in agricultural soils and have many traits that make them well suited as biocontrol agents of soilborne pathogens. Tremendous progress has been made in characterizing the process of root colonization by pseudomonads, the biotic and abiotic factors affecting colonization, bacterial traits and genes contributing to rhizosphere competence, and the mechanisms of pathogen suppression. This review looks back over the last 30 years of Pseudomonas biocontrol research and highlights key studies, strains, and findings that have had significant impact on shaping our current understanding of biological control by bacteria and the direction of future research.


1998 ◽  
Vol 29 (9-10) ◽  
pp. 1239-1251 ◽  
Author(s):  
D. G. Dimoyiannis ◽  
C. D. Tsadilas ◽  
S. Valmis

2021 ◽  
Author(s):  
Iqbal Ahmad ◽  
Bushra Khan ◽  
Nida Gul ◽  
Muhammad Khan ◽  
Javaid Iqbal ◽  
...  

Abstract Lead (Pb) contamination in soil and subsequent transport in groundwater poses severe threats to the food safety and human health. In current study, the effects of soil organic matter on sorption behavior of Pb onto six agricultural soils were investigated by batch sorption experiments and microscopic characterization. Results indicated that Pb sorption onto agricultural soils was dominated by the soil organic matter content and soil texture. The decrease of organic matter content reduced the sorption capacity of Pb onto agricultural soils. Based on soil texture, the Pb sorption was highest in clay soil and lowest in silt type of soil. The overall Pb sorption was in the order of clay > clay loam > silty clay loam ≈ loam > silt loam > silt. The sorption isotherms of measured aqueous and soil phase Pb concentrations were fit well with the linear sorption model. The organic carbon normalized partition coefficients (Log KOC) ranged from 2.90 to 2.99. Linear partition coefficient (Kd) values were positively correlated with the soil properties, such as clay (R2 =0.90), OC (R2 =0.94) and pH (R2 = 0.45); however, weak correlation was found between Kd and soil sand contents (R2 = 0.12). The leachability model showed potential risk of Pb leaching from silt soil with lowest organic matter content. The findings are of significant importance for understanding potential threats of Pb to the soil ecosystem, groundwater, plants, and humans.


2009 ◽  
Vol 28 (12) ◽  
pp. 2546 ◽  
Author(s):  
Sara C. Monteiro ◽  
Alistair B.A. Boxall

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