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Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format Example of Plant and Soil format
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open access Open Access
recommended Recommended

Plant and Soil — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Plant Science #33 of 445 up up by 3 ranks
Soil Science #19 of 135 down down by 4 ranks
journal-quality-icon Journal quality:
High
calendar-icon Last 4 years overview: 1626 Published Papers | 10282 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 03/07/2020
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Related Journals

open access Open Access
recommended Recommended

Elsevier

Quality:  
High
CiteRatio: 8.6
SJR: 1.684
SNIP: 2.192
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Wiley

Quality:  
High
CiteRatio: 9.0
SJR: 1.945
SNIP: 1.683
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Wiley

Quality:  
Good
CiteRatio: 3.3
SJR: 0.644
SNIP: 0.761
open access Open Access
recommended Recommended

Taylor and Francis

Quality:  
High
CiteRatio: 9.2
SJR: 1.713
SNIP: 2.207

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.

3.299

1% from 2018

Impact factor for Plant and Soil from 2016 - 2019
Year Value
2019 3.299
2018 3.259
2017 3.306
2016 3.052
graph view Graph view
table view Table view

6.3

7% from 2019

CiteRatio for Plant and Soil from 2016 - 2020
Year Value
2020 6.3
2019 5.9
2018 5.4
2017 5.8
2016 6.3
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has increased by 1% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • CiteRatio of this journal has increased by 7% 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.

1.28

6% from 2019

SJR for Plant and Soil from 2016 - 2020
Year Value
2020 1.28
2019 1.208
2018 1.187
2017 1.361
2016 1.295
graph view Graph view
table view Table view

1.36

6% from 2019

SNIP for Plant and Soil from 2016 - 2020
Year Value
2020 1.36
2019 1.285
2018 1.261
2017 1.484
2016 1.47
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has increased by 6% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has increased by 6% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

Plant and Soil

Guideline source: View

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Springer

Plant and Soil

Plant and Soil publishes original papers and review articles exploring the interface of plant biology and soil sciences, and that enhance our mechanistic understanding of plant-soil interactions. We focus on the interface of plant biology and soil sciences, and seek those manu...... Read More

i
Last updated on
03 Jul 2020
i
ISSN
0032-079X
i
Impact Factor
High - 1.442
i
Acceptance Rate
Not provided
i
Frequency
Not provided
i
Open Access
Yes
i
Sherpa RoMEO Archiving Policy
Green faq
i
Plagiarism Check
Available via Turnitin
i
Endnote Style
Download Available
i
Citation Type
Author Year
(Blonder et al, 1982)
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Bibliography Example
Beenakker CWJ (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: 10.1007/BF00018060
Rapid determination of free proline for water-stress studies
L. S. Bates1, R. P. Waldren1, I. D. Teare1
01 Aug 1973 - Plant and Soil

Abstract:

Proline, which increases proportionately faster than other amino acids in plants under water stress, has been suggested as an evaluating parameter for irrigation scheduling and for selecting drought-resistant varieties. The necessity to analyze numerous samples from multiple replications of field grown materials prompted the ... Proline, which increases proportionately faster than other amino acids in plants under water stress, has been suggested as an evaluating parameter for irrigation scheduling and for selecting drought-resistant varieties. The necessity to analyze numerous samples from multiple replications of field grown materials prompted the development of a simple, rapid colorimetric determination of proline. The method detected proline in the 0.1 to 36.0 μmoles/g range of fresh weight leaf material. read more read less

Topics:

Proline dehydrogenase activity (68%)68% related to the paper, Proline oxidase activity (68%)68% related to the paper, Proline dehydrogenase (59%)59% related to the paper, Proline oxidase (57%)57% related to the paper, Proline (53%)53% related to the paper
15,328 Citations
Journal Article DOI: 10.1023/A:1016125726789
Stabilization mechanisms of soil organic matter: Implications for C-saturation of soils
Johan Six1, Richard T. Conant1, Eldor A. Paul1, Keith Paustian1
01 Apr 2002 - Plant and Soil

Abstract:

The relationship between soil structure and the ability of soil to stabilize soil organic matter (SOM) is a key element in soil C dynamics that has either been overlooked or treated in a cursory fashion when developing SOM models. The purpose of this paper is to review current knowledge of SOM dynamics within the framework of... The relationship between soil structure and the ability of soil to stabilize soil organic matter (SOM) is a key element in soil C dynamics that has either been overlooked or treated in a cursory fashion when developing SOM models. The purpose of this paper is to review current knowledge of SOM dynamics within the framework of a newly proposed soil C saturation concept. Initially, we distinguish SOM that is protected against decomposition by various mechanisms from that which is not protected from decomposition. Methods of quantification and characteristics of three SOM pools defined as protected are discussed. Soil organic matter can be: (1) physically stabilized, or protected from decomposition, through microaggregation, or (2) intimate association with silt and clay particles, and (3) can be biochemically stabilized through the formation of recalcitrant SOM compounds. In addition to behavior of each SOM pool, we discuss implications of changes in land management on processes by which SOM compounds undergo protection and release. The characteristics and responses to changes in land use or land management are described for the light fraction (LF) and particulate organic matter (POM). We defined the LF and POM not occluded within microaggregates (53–250 μm sized aggregates as unprotected. Our conclusions are illustrated in a new conceptual SOM model that differs from most SOM models in that the model state variables are measurable SOM pools. We suggest that physicochemical characteristics inherent to soils define the maximum protective capacity of these pools, which limits increases in SOM (i.e. C sequestration) with increased organic residue inputs. read more read less

Topics:

Soil organic matter (63%)63% related to the paper, Soil structure (52%)52% related to the paper, Soil water (51%)51% related to the paper
3,301 Citations
Journal Article DOI: 10.1023/A:1026037216893
Plant growth promoting rhizobacteria as biofertilizers
J. Kevin Vessey1
16 Mar 2003 - Plant and Soil

Abstract:

Numerous species of soil bacteria which flourish in the rhizosphere of plants, but which may grow in, on, or around plant tissues, stimulate plant growth by a plethora of mechanisms. These bacteria are collectively known as PGPR (plant growth promoting rhizobacteria). The search for PGPR and investigation of their modes of ac... Numerous species of soil bacteria which flourish in the rhizosphere of plants, but which may grow in, on, or around plant tissues, stimulate plant growth by a plethora of mechanisms. These bacteria are collectively known as PGPR (plant growth promoting rhizobacteria). The search for PGPR and investigation of their modes of action are increasing at a rapid pace as efforts are made to exploit them commercially as biofertilizers. After an initial clarification of the term biofertilizers and the nature of associations between PGPR and plants (i.e., endophytic versus rhizospheric), this review focuses on the known, the putative, and the speculative modes-of-action of PGPR. These modes of action include fixing N2, increasing the availability of nutrients in the rhizosphere, positively influencing root growth and morphology, and promoting other beneficial plant–microbe symbioses. The combination of these modes of actions in PGPR is also addressed, as well as the challenges facing the more widespread utilization of PGPR as biofertilizers. read more read less

Topics:

Rhizobacteria (55%)55% related to the paper, Biofertilizer (52%)52% related to the paper, Rhizosphere (51%)51% related to the paper
2,982 Citations
Journal Article DOI: 10.1023/A:1004356007312
Organic acids in the rhizosphere: a critical review
David L. Jones1
01 Dec 1998 - Plant and Soil

Abstract:

Organic acids, such as malate, citrate and oxalate, have been proposed to be involved in many processes operating in the rhizosphere, including nutrient acquisition and metal detoxification, alleviation of anaerobic stress in roots, mineral weathering and pathogen attraction. A full assessment of their role in these processes... Organic acids, such as malate, citrate and oxalate, have been proposed to be involved in many processes operating in the rhizosphere, including nutrient acquisition and metal detoxification, alleviation of anaerobic stress in roots, mineral weathering and pathogen attraction. A full assessment of their role in these processes, however, cannot be determined unless the exact mechanisms of plant organic acid release and the fate of these compounds in the soil are more fully understood. This review therefore includes information on organic acid levels in plants (concentrations, compartmentalisation, spatial aspects, synthesis), plant efflux (passive versus active transport, theoretical versus experimental considerations), soil reactions (soil solution concentrations, sorption) and microbial considerations (mineralization). In summary, the release of organic acids from roots can operate by multiple mechanisms in response to a number of well-defined environmental stresses (e.g., Al, P and Fe stress, anoxia): These responses, however, are highly stress- and plant-species specific. In addition, this review indicates that the sorption of organic acids to the mineral phase and mineralisation by the soil's microbial biomass are critical to determining the effectiveness of organic acids in most rhizosphere processes. read more read less

Topics:

Rhizosphere (60%)60% related to the paper, Soil organic matter (58%)58% related to the paper, Organic acid (58%)58% related to the paper, Mineralization (soil science) (57%)57% related to the paper
2,339 Citations
Journal Article DOI: 10.1023/A:1013351617532
Bioavailability of soil inorganic P in the rhizosphere as affected by root-induced chemical changes: A review
Philippe Hinsinger1
04 Apr 2001 - Plant and Soil

Abstract:

In most soils, inorganic phosphorus occurs at fairly low concentrations in the soil solution whilst a large proportion of it is more or less strongly held by diverse soil minerals. Phosphate ions can indeed be adsorbed onto positively charged minerals such as Fe and Al oxides. Phosphate (P) ions can also form a range of miner... In most soils, inorganic phosphorus occurs at fairly low concentrations in the soil solution whilst a large proportion of it is more or less strongly held by diverse soil minerals. Phosphate ions can indeed be adsorbed onto positively charged minerals such as Fe and Al oxides. Phosphate (P) ions can also form a range of minerals in combination with metals such as Ca, Fe and Al. These adsorption/desorption and precipitation/dissolution equilibria control the concentration of P in the soil solution and, thereby, both its chemical mobility and bioavailability. Apart from the concentration of P ions, the major factors that determine those equilibria as well as the speciation of soil P are (i) the pH, (ii) the concentrations of anions that compete with P ions for ligand exchange reactions and (iii) the concentrations of metals (Ca, Fe and Al) that can coprecipitate with P ions. The chemical conditions of the rhizosphere are known to considerably differ from those of the bulk soil, as a consequence of a range of processes that are induced either directly by the activity of plant roots or by the activity of rhizosphere microflora. The aim of this paper is to give an overview of those chemical processes that are directly induced by plant roots and which can affect the concentration of P in the soil solution and, ultimately, the bioavailability of soil inorganic P to plants. Amongst these, the uptake activity of plant roots should be taken into account in the first place. A second group of activities which is of major concern with respect to P bioavailability are those processes that can affect soil pH, such as proton/bicarbonate release (anion/cation balance) and gaseous (O2/CO2) exchanges. Thirdly, the release of root exudates such as organic ligands is another activity of the root that can alter the concentration of P in the soil solution. These various processes and their relative contributions to the changes in the bioavailability of soil inorganic P that can occur in the rhizosphere can considerably vary with (i) plant species, (ii) plant nutritional status and (iii) ambient soil conditions, as will be stressed in this paper. Their possible implications for the understanding and management of P nutrition of plants will be briefly addressed and discussed. read more read less

Topics:

Bulk soil (65%)65% related to the paper, Soil chemistry (62%)62% related to the paper, Rhizosphere (61%)61% related to the paper, Soil pH (59%)59% related to the paper, Soil water (55%)55% related to the paper
2,120 Citations
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Frequently asked questions

1. Can I write Plant and Soil in LaTeX?

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

2. Do you follow the Plant and Soil guidelines?

Yes, the template is compliant with the Plant and Soil 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 Plant and Soil?

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 Plant and Soil citation style.

4. Can I use the Plant and Soil 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 Plant and Soil.

5. Can I use a manuscript in Plant and Soil 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 Plant and Soil that you can download at the end.

6. How long does it usually take you to format my papers in Plant and Soil?

It only takes a matter of seconds to edit your manuscript. Besides that, our intuitive editor saves you from writing and formatting it in Plant and Soil.

7. Where can I find the template for the Plant and Soil?

It is possible to find the Word template for any journal on Google. However, why use a template when you can write your entire manuscript on SciSpace , auto format it as per Plant and Soil's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

8. Can I reformat my paper to fit the Plant and Soil's guidelines?

Of course! You can do this using our intuitive editor. It's very easy. If you need help, our support team is always ready to assist you.

9. Plant and Soil an online tool or is there a desktop version?

SciSpace's Plant and Soil is currently available as an online tool. We're developing a desktop version, too. You can request (or upvote) any features that you think would be helpful for you and other researchers in the "feature request" section of your account once you've signed up with us.

10. I cannot find my template in your gallery. Can you create it for me like Plant and Soil?

Sure. You can request any template and we'll have it setup within a few days. You can find the request box in Journal Gallery on the right side bar under the heading, "Couldn't find the format you were looking for like Plant and Soil?”

11. What is the output that I would get after using Plant and Soil?

After writing your paper autoformatting in Plant and Soil, you can download it in multiple formats, viz., PDF, Docx, and LaTeX.

12. Is Plant and Soil'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 Plant and Soil?

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 Plant and Soil. 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 Plant and Soil?

The 5 most common citation types in order of usage for Plant and Soil 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 Plant and Soil?

It is possible to find the Word template for any journal on Google. However, why use a template when you can write your entire manuscript on SciSpace , auto format it as per Plant and Soil's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

16. Can I download Plant and Soil 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 Plant and Soil Endnote style according to Elsevier guidelines.

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