Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Concept Videos

The Soil Ecosystem02:23

The Soil Ecosystem

24.3K
Plants obtain inorganic minerals and water from the soil, which acts as a natural medium for land plants. The composition and quality of soil depend not only on the chemical constituents but also on the presence of living organisms. In general, soils contain three major components:
24.3K
Primary Production01:06

Primary Production

25.0K
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
25.0K

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

Uncovering plant root traits and mechanisms that enable penetration, exploration, and exploitation of soil parent materials: a systematic review.

Plant and soil·2026
Same author

New Oldowan locality Sare-Abururu (ca. 1.7 Ma) provides evidence of diverse hominin behaviors on the Homa Peninsula, Kenya.

Journal of human evolution·2024
Same author

How the EU Soil Observatory contributes to a stronger soil erosion community.

Environmental research·2024
Same author

How Much Food Can We Grow in Urban Areas? Food Production and Crop Yields of Urban Agriculture: A Meta-Analysis.

Earth's future·2022

Related Experiment Video

Updated: Dec 29, 2025

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
11:19

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses

Published on: October 21, 2016

12.3K

Cosmogenic soil production rate calculator.

Ángel Rodés1, Daniel L Evans2

  • 1Scottish Universities Environmental Research Centre, East Kilbride, UK.

Methodsx
|February 6, 2020
PubMed
Summary

New soil production models calculate bedrock erosion rates more accurately by accounting for varying soil densities. This improves our understanding of soil formation and landscape evolution.

Keywords:
10Be14C21Ne26Al36Cl3HeCosmogenic nuclidesCosmogenic soil production rate calculator (CoSOILcal)Erosion rateMATLABOctaveSoil production

More Related Videos

Use of Principal Components for Scaling Up Topographic Models to Map Soil Redistribution and Soil Organic Carbon
09:44

Use of Principal Components for Scaling Up Topographic Models to Map Soil Redistribution and Soil Organic Carbon

Published on: October 16, 2018

10.6K
Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
07:32

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

Published on: June 4, 2021

5.6K

Related Experiment Videos

Last Updated: Dec 29, 2025

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
11:19

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses

Published on: October 21, 2016

12.3K
Use of Principal Components for Scaling Up Topographic Models to Map Soil Redistribution and Soil Organic Carbon
09:44

Use of Principal Components for Scaling Up Topographic Models to Map Soil Redistribution and Soil Organic Carbon

Published on: October 16, 2018

10.6K
Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
07:32

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

Published on: June 4, 2021

5.6K

Area of Science:

  • Geomorphology
  • Soil Science
  • Cosmogenic Nuclide Geochronology

Background:

  • Understanding soil formation rates is crucial for quantifying landscape evolution.
  • Previous models for apparent erosion rates assumed constant or bedrock-equivalent soil bulk density.
  • These assumptions are flawed as soil densities are typically lower and vary with depth.

Purpose of the Study:

  • To develop a novel model for calculating isotopically-derived soil production rates.
  • To incorporate soil bulk density profiles into the calculation of erosion rates.
  • To provide a more accurate method for understanding bedrock lowering.

Main Methods:

  • Utilized measured concentrations of cosmogenic radionuclides.
  • Developed a new model that accounts for the bulk density profile of the overlying soil.
  • Implemented the model in MATLAB® and GNU Octave© for accessibility.

Main Results:

  • The new model allows for the calculation of soil production rates considering variable soil densities.
  • This addresses a key limitation of previous erosion rate models.
  • The model provides a more realistic estimation of bedrock surface lowering.

Conclusions:

  • The developed model offers a significant advancement in deriving accurate soil production rates.
  • Accounting for soil bulk density profiles enhances the reliability of cosmogenic nuclide-based erosion estimates.
  • This contributes to a better understanding of soil formation processes and landscape dynamics.