Your Gateway to Smarter Soil Solutions
Media Hub
Explore our growing library of podcasts and videos designed to bring soil science to life. Hear directly from farmers, researchers, and industry experts as they share real-world experiences, practical strategies, and the latest innovations in soil management.
Whether you prefer to listen on the go or watch in-depth demonstrations, the Media Hub makes it easy to learn in a way that suits you.
Explore Key Categories
Browse by Media Type
Find Content Your Way
Filter content based on how you like to learn: Podcasts – Listen to conversations, interviews, and expert discussions Or Videos – Watch demonstrations, case studies, and field insights.
Active filters
Promote Your Project on Soils Connect
Share your insights, innovations, and success stories with a community dedicated to soil health and sustainable farming. Highlight your project, inspire change, and connect with farmers, researchers, and advisors across the region.
Latest
Helpful tools
Explore a range of helpful tools designed to simplify soil management, from interactive calculators to step-by-step guides tailored to your farming needs.
Can’t find what you’re looking for?
Practical Tools & Resources
Resource Hub
The Resource Hub brings together practical, evidence-based information you can apply on-farm — from step-by-step guides and case studies to calculators and technical resources.
Whether you’re tackling a specific soil constraint or looking to improve long-term productivity, you’ll find resources tailored to your needs.
Q40. What is it about soil texture that impacts growth? Especially in a crop like lentils?
Soil texture significantly affects crop growth by influencing water retention, nutrient storage, and drainage; lentils particularly prefer loamy soils due to their balanced moisture availability and nutrient-holding capacity, and dislike acidic or waterlogged conditions.
View more
Q39. When one patch of sandy soil starts eroding, will the patch of erosion grow and grow until you are left with a large unproductive area of soil?
Unchecked erosion on sandy soils can rapidly expand and degrade surrounding areas, so maintaining permanent vegetative cover, managing soil constraints, and minimising disturbance are essential to prevent extensive erosion.
View more
Q38. Why are sandy soils different across South Australia?
Sandy soils differ across South Australia due to variations in their geological origins, age, parent material, climate, and land management history, resulting in distinct properties like pH, texture, depth to clay, and nutrient availability.
View more
Q34. Is there any benefit to deep ripping clay loams?
Deep ripping clay loams offers limited and unpredictable benefits, with potential risks of bringing hostile subsoil (dispersive, saline, or boron-rich) to the surface; a careful test rip is recommended first.
View more
Q33. Why would I deep rip my sandy soils? Will I get a yield response?
Deep ripping dispersive soil is generally not recommended without gypsum, as benefits are short-lived and ripping may worsen dispersion, salinity, or boron issues.
View more
Q25. Can I rip into dispersive soil to open it up?
Deep ripping dispersive soil is generally not recommended without gypsum, as benefits are short-lived and ripping may worsen dispersion, salinity, or boron issues.
View more
Got a question for Soils Connect?
Visit our question library and learn more, if your question hasn’t been asked, submit your question here and we will get back to you with an informative answer.
Frequently asked questions
What is Soils Connect?
Soils Connect is your one-stop shop for everything soil! I’m here to help you explore tools, guides, and resources to keep your soil healthy, productive, and ready to handle whatever Mother Nature throws your way!
Who can use Soils Connect?
Content goes here ..
What resources can I find on Soils Connect?
Content goes here ..
Is Soils Connect free to use?
Content goes here ..
How do I ask a question or get expert advice?
Content goes here ..
How can I get started with Soils Connect?
Content goes here ..


