Example of European Journal of Soil Science format
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Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format
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Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format Example of European Journal of Soil Science format
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open access Open Access

European Journal of Soil Science — Template for authors

Publisher: Wiley
Categories Rank Trend in last 3 yrs
Soil Science #17 of 135 down down by 4 ranks
journal-quality-icon Journal quality:
High
calendar-icon Last 4 years overview: 378 Published Papers | 2534 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 11/06/2020
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Journal Performance & Insights

Impact Factor

CiteRatio

Determines the importance of a journal by taking a measure of frequency with which the average article in a journal has been cited in a particular year.

A measure of average citations received per peer-reviewed paper published in the journal.

3.742

33% from 2018

Impact factor for European Journal of Soil Science from 2016 - 2019
Year Value
2019 3.742
2018 2.818
2017 2.644
2016 3.475
graph view Graph view
table view Table view

6.7

29% from 2019

CiteRatio for European Journal of Soil Science from 2016 - 2020
Year Value
2020 6.7
2019 5.2
2018 5.1
2017 6.1
2016 5.7
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has increased by 33% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • CiteRatio of this journal has increased by 29% in last years.
  • This journal’s CiteRatio is in the top 10 percentile category.

SCImago Journal Rank (SJR)

Source Normalized Impact per Paper (SNIP)

Measures weighted citations received by the journal. Citation weighting depends on the categories and prestige of the citing journal.

Measures actual citations received relative to citations expected for the journal's category.

1.244

2% from 2019

SJR for European Journal of Soil Science from 2016 - 2020
Year Value
2020 1.244
2019 1.267
2018 1.116
2017 1.44
2016 1.426
graph view Graph view
table view Table view

1.482

2% from 2019

SNIP for European Journal of Soil Science from 2016 - 2020
Year Value
2020 1.482
2019 1.506
2018 1.249
2017 1.321
2016 1.498
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has decreased by 2% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has decreased by 2% in last years.
  • This journal’s SNIP is in the top 10 percentile category.
European Journal of Soil Science

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Wiley

European Journal of Soil Science

Our understanding of soil continues to advance. Better instruments and new techniques allow us to penetrate its structure and monitor its behaviour. Developments in statistical theory backed by sound programming and more powerful computers are leading to more effective survey ...... Read More

Soil Science

Agricultural and Biological Sciences

i
Last updated on
11 Jun 2020
i
ISSN
1351-0754
i
Impact Factor
High - 1.557
i
Open Access
Yes
i
Sherpa RoMEO Archiving Policy
Yellow faq
i
Plagiarism Check
Available via Turnitin
i
Endnote Style
Download Available
i
Bibliography Name
apa
i
Citation Type
Numbered
[25]
i
Bibliography Example
Beenakker, C.W.J. (2006) Specular andreev reflection in graphene.Phys. Rev. Lett., 97 (6), 067 007. URL 10.1103/PhysRevLett.97.067007.

Top papers written in this journal

Journal Article DOI: 10.1111/J.1365-2389.1982.TB01755.X
Organic matter and water-stable aggregates in soils
Judith. Tisdall1, J.M. Oades1

Abstract:

Summary The water-stability of aggregates in many soils is shown to depend on organic materials. The organic binding agents have been classified into (a) transient, mainly polysaccharides, (b), temporary, roots and fungal hyphae, and (c) persistent, resistant aromatic components associated with polyvalent metal cations, and ... Summary The water-stability of aggregates in many soils is shown to depend on organic materials. The organic binding agents have been classified into (a) transient, mainly polysaccharides, (b), temporary, roots and fungal hyphae, and (c) persistent, resistant aromatic components associated with polyvalent metal cations, and strongly sorbed polymers. The effectiveness of various binding agents at different stages in the structural organization of aggregates is described and forms the basis of a model which illustrates the architecture of an aggregate. Roots and hyphae stabilize macro-aggregates, defined as > 250 μm diameter; consequently, macroaggregation is controlled by soil management (i.e. crop rotations), as management influences the growth of plant roots, and the oxidation of organic carbon. The water-stability of micro-aggregates depends on the persistent organic binding agents and appears to be a characteristic of the soil, independent of management. read more read less

Topics:

Organic matter (57%)57% related to the paper, Glomalin (51%)51% related to the paper
5,389 Citations
Journal Article DOI: 10.1111/EJSS.12114_2
Total carbon and nitrogen in the soils of the world
Niels H. Batjes1

Abstract:

Summary The soil is important in sequestering atmospheric CO2 and in emitting trace gases (e.g. CO2, CH4 and N2O) that are radiatively active and enhance the ‘greenhouse’ effect. Land use changes and predicted global warming, through their effects on net primary productivity, the plant community and soil conditions, may have... Summary The soil is important in sequestering atmospheric CO2 and in emitting trace gases (e.g. CO2, CH4 and N2O) that are radiatively active and enhance the ‘greenhouse’ effect. Land use changes and predicted global warming, through their effects on net primary productivity, the plant community and soil conditions, may have important effects on the size of the organic matter pool in the soil and directly affect the atmospheric concentration of these trace gases. A discrepancy of approximately 350 × 1015 g (or Pg) of C in two recent estimates of soil carbon reserves worldwide is evaluated using the geo-referenced database developed for the World Inventory of Soil Emission Potentials (WISE) project. This database holds 4353 soil profiles distributed globally which are considered to represent the soil units shown on a 1/2° latitude by 1/2° longitude version of the corrected and digitized 1:5 M FAO–UNESCO Soil Map of the World. Total soil carbon pools for the entire land area of the world, excluding carbon held in the litter layer and charcoal, amounts to 2157–2293 Pg of C in the upper 100 cm. Soil organic carbon is estimated to be 684–724 Pg of C in the upper 30 cm, 1462–1548 Pg of C in the upper 100 cm, and 2376–2456 Pg of C in the upper 200 cm. Although deforestation, changes in land use and predicted climate change can alter the amount of organic carbon held in the superficial soil layers rapidly, this is less so for the soil carbonate carbon. An estimated 695–748 Pg of carbonate-C is held in the upper 100 cm of the world's soils. Mean C: N ratios of soil organic matter range from 9.9 for arid Yermosols to 25.8 for Histosols. Global amounts of soil nitrogen are estimated to be 133–140 Pg of N for the upper 100 cm. Possible changes in soil organic carbon and nitrogen dynamics caused by increased concentrations of atmospheric CO2 and the predicted associated rise in temperature are discussed. read more read less

Topics:

Soil organic matter (72%)72% related to the paper, Soil carbon (69%)69% related to the paper, Soil biology (65%)65% related to the paper, Histosol (64%)64% related to the paper, Soil horizon (64%)64% related to the paper
View PDF
3,163 Citations
Journal Article DOI: 10.1111/J.1365-2389.2006.00809.X
Stabilization of organic matter in temperate soils: mechanisms and their relevance under different soil conditions – a review

Abstract:

Summary Mechanisms for C stabilization in soils have received much interest recently due to their relevance in the global C cycle. Here we review the mechanisms that are currently, but often contradictorily or inconsistently, considered to contribute to organic matter (OM) protection against decomposition in temperate soils:... Summary Mechanisms for C stabilization in soils have received much interest recently due to their relevance in the global C cycle. Here we review the mechanisms that are currently, but often contradictorily or inconsistently, considered to contribute to organic matter (OM) protection against decomposition in temperate soils: (i) selective preservation due to recalcitrance of OM, including plant litter, rhizodeposits, microbial products, humic polymers, and charred OM; (ii) spatial inaccessibility of OM against decomposer organisms due to occlusion, intercalation, hydrophobicity and encapsulation; and (iii) stabilization by interaction with mineral surfaces (Fe-, Al-, Mn-oxides, phyllosilicates) and metal ions. Our goal is to assess the relevance of these mechanisms to the formation of soil OM during different stages of decomposition and under different soil conditions. The view that OM stabilization is dominated by the selective preservation of recalcitrant organic components that accumulate in proportion to their chemical properties can no longer be accepted. In contrast, our analysis of mechanisms shows that: (i) the soil biotic community is able to disintegrate any OM of natural origin; (ii) molecular recalcitrance of OM is relative, rather than absolute; (iii) recalcitrance is only important during early decomposition and in active surface soils; while (iv) during late decomposition and in the subsoil, the relevance of spatial inaccessibility and organo-mineral interactions for SOM stabilization increases. We conclude that major difficulties in the understanding and prediction of SOM dynamics originate from the simultaneous operation of several mechanisms. We discuss knowledge gaps and promising directions of future research. read more read less

Topics:

Organic matter (51%)51% related to the paper
2,332 Citations
Journal Article DOI: 10.1111/EJSS.4_12398
Microbial diversity and soil functions

Abstract:

Summary Soil is a complex and dynamic biological system, and still in 2003 it is difficult to determine the composition of microbial communities in soil. We are also limited in the determination of microbially mediated reactions because present assays for determining the overall rate of entire metabolic processes (such as re... Summary Soil is a complex and dynamic biological system, and still in 2003 it is difficult to determine the composition of microbial communities in soil. We are also limited in the determination of microbially mediated reactions because present assays for determining the overall rate of entire metabolic processes (such as respiration) or specific enzyme activities (such as urease, protease and phosphomonoesterase activity) do not allow any identification of the microbial species directly involved in the measured processes. The central problem posed by the link between microbial diversity and soil function is to understand the relations between genetic diversity and community structure and between community structure and function. A better understanding of the relations between microbial diversity and soil functions requires not only the use of more accurate assays for taxonomically and functionally characterizing DNA and RNA extracted from soil, but also high-resolution techniques with which to detect inactive and active microbial cells in the soil matrix. Soil seems to be characterized by a redundancy of functions; for example, no relationship has been shown to exist between microbial diversity and decomposition of organic matter. Generally, a reduction in any group of species has little effect on overall processes in soil because other microorganisms can take on its function. The determination of the composition of microbial communities in soil is not necessary for a better quantification of nutrient transformations. The holistic approach, based on the division of the systems in pools and the measurement of fluxes linking these pools, is the most efficient. The determination of microbial C, N, P and S contents by fumigation techniques has allowed a better quantification of nutrient dynamics in soil. However, further advances require determining new pools, such as active microbial biomass, also with molecular techniques. Recently investigators have separated 13C- and 12C-DNA, both extracted from soil treated with a 13C source, by density-gradient centrifugation. This technique should allow us to calculate the active microbial C pool by multiplying the ratio between labelled and total DNA by the microbial biomass C content of soil. In addition, the taxonomic and functional characterization of 13C-DNA allows us to understand more precisely the changes in the composition of microbial communities affected by the C-substrate added to soil. read more read less

Topics:

Soil functions (60%)60% related to the paper, Microbial population biology (53%)53% related to the paper
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1,887 Citations
Journal Article DOI: 10.1111/J.1365-2389.1996.TB01843.X
Aggregate stability and assessment of soil crustability and erodibility: I. Theory and methodology
Y. Le Bissonnais1

Abstract:

Summary Crusting and erosion of cultivated soils result from aggregate breakdown and the detachment of soil fragments by rain, and the susceptibility of soil to these processes is often inferred from measurements of aggregate stability. Here, theories of aggregate breakdown are reviewed and four main mechanisms (i.e. slaking... Summary Crusting and erosion of cultivated soils result from aggregate breakdown and the detachment of soil fragments by rain, and the susceptibility of soil to these processes is often inferred from measurements of aggregate stability. Here, theories of aggregate breakdown are reviewed and four main mechanisms (i.e. slaking, breakdown by differential swelling, mechanical breakdown by raindrop impact and physico–chemical dispersion) are defined. Their relative importance depends on the nature of the rain, as well as on the soil's physical and chemical properties. The relations between aggregate breakdown, crusting and water erosion are analysed, and existing methods for the assessment of aggregate stability are reviewed. A unified framework for the measurement of aggregate stability is proposed to assess a soil's susceptibility to crusting and erosion. It combines three treatments having various wetting conditions and energies (fast wetting, slow wetting, and stirring after pre-wetting) and measures the resulting fragment size distribution after each treatment. It is designed to compare different soils, or different climatic conditions for a given soil, not to compare time-dependent changes in that soil. read more read less

Topics:

Dispersion (geology) (53%)53% related to the paper, Erosion (53%)53% related to the paper, Aggregate (composite) (51%)51% related to the paper, Soil water (51%)51% related to the paper
1,259 Citations
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Frequently asked questions

1. Can I write European Journal of Soil Science in LaTeX?

Absolutely not! Our tool has been designed to help you focus on writing. You can write your entire paper as per the European Journal of Soil Science guidelines and auto format it.

2. Do you follow the European Journal of Soil Science guidelines?

Yes, the template is compliant with the European Journal of Soil Science guidelines. Our experts at SciSpace ensure that. If there are any changes to the journal's guidelines, we'll change our algorithm accordingly.

3. Can I cite my article in multiple styles in European Journal of Soil Science?

Of course! We support all the top citation styles, such as APA style, MLA style, Vancouver style, Harvard style, and Chicago style. For example, when you write your paper and hit autoformat, our system will automatically update your article as per the European Journal of Soil Science citation style.

4. Can I use the European Journal of Soil Science templates for free?

Sign up for our free trial, and you'll be able to use all our features for seven days. You'll see how helpful they are and how inexpensive they are compared to other options, Especially for European Journal of Soil Science.

5. Can I use a manuscript in European Journal of Soil Science that I have written in MS Word?

Yes. You can choose the right template, copy-paste the contents from the word document, and click on auto-format. Once you're done, you'll have a publish-ready paper European Journal of Soil Science that you can download at the end.

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7. Where can I find the template for the European Journal of Soil Science?

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8. Can I reformat my paper to fit the European Journal of Soil Science's guidelines?

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12. Is European Journal of Soil Science's impact factor high enough that I should try publishing my article there?

To be honest, the answer is no. The impact factor is one of the many elements that determine the quality of a journal. Few of these factors include review board, rejection rates, frequency of inclusion in indexes, and Eigenfactor. You need to assess all these factors before you make your final call.

13. What is Sherpa RoMEO Archiving Policy for European Journal of Soil Science?

SHERPA/RoMEO Database

We extracted this data from Sherpa Romeo to help researchers understand the access level of this journal in accordance with the Sherpa Romeo Archiving Policy for European Journal of Soil Science. The table below indicates the level of access a journal has as per Sherpa Romeo's archiving policy.

RoMEO Colour Archiving policy
Green Can archive pre-print and post-print or publisher's version/PDF
Blue Can archive post-print (ie final draft post-refereeing) or publisher's version/PDF
Yellow Can archive pre-print (ie pre-refereeing)
White Archiving not formally supported
FYI:
  1. Pre-prints as being the version of the paper before peer review and
  2. Post-prints as being the version of the paper after peer-review, with revisions having been made.

14. What are the most common citation types In European Journal of Soil Science?

The 5 most common citation types in order of usage for European Journal of Soil Science are:.

S. No. Citation Style Type
1. Author Year
2. Numbered
3. Numbered (Superscripted)
4. Author Year (Cited Pages)
5. Footnote

15. How do I submit my article to the European Journal of Soil Science?

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16. Can I download European Journal of Soil Science in Endnote format?

Yes, SciSpace provides this functionality. After signing up, you would need to import your existing references from Word or Bib file to SciSpace. Then SciSpace would allow you to download your references in European Journal of Soil Science Endnote style according to Elsevier guidelines.

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