Author: GAEA Technologies
Posts
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Upgrade to POLLUTE and MIGRATE Version 10
POLLUTE & MIGRATE — Modern Contaminant Modeling Platform Move beyond legacy tools and unlock integrated 1D + 2D modeling, GIS visualization, and modern workflows. 👉 Upgrade Now 👉 View Features Still Using POLLUTE v7 or MIGRATE v9? Introducing POLLUTE and MIGRATE Version 10 A unified platform combining modeling, visualization, and data management. See POLLUTEv10 in…
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Upgrade to WinLoG v6 — Faster Workflows, Better Results
Still using WinLoG v4? Save time on every project with faster data entry, cleaner outputs, and smarter workflows in GaeaSynergy. 👉 Upgrade Now 👉 View Features Trusted by geotechnical and environmental professionals • Backward compatible • Proven workflows Still Using WinLoG v4? Here’s the Hidden Cost. WinLoG v4 still works—but it’s costing you time on…
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How to Build a Breakthrough Curve for Contaminant Transport
Breakthrough curves are one of the most powerful tools in contaminant hydrogeology. Whether you’re assessing landfill leachate migration, evaluating remediation performance, or modeling groundwater contamination, a well-constructed breakthrough curve provides clear insight into how contaminants move through subsurface systems over time. In 2026, the process goes beyond spreadsheets. With advanced tools like POLLUTE and MIGRATE,…
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How to Reduce Borehole Logging Time by 70% Using Digital Workflows (2026 Guide)
Borehole logging has long been one of the most time-intensive tasks in environmental and geotechnical consulting. Between handwritten field notes, spreadsheet transcription, log drafting, and report formatting, it’s common for projects to spend more time processing data than actually collecting it. But leading firms are changing that. By implementing fully digital workflows—especially using tools like…
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MIGRATEv10: A Powerful New Standard in 2D Contaminant Transport Modeling
GAEA Technologies is proud to announce the release of MIGRATEv10, the latest evolution in contaminant transport modeling software designed to deliver enhanced accuracy, flexibility, and insight for environmental professionals. MIGRATEv10 introduces advanced two-dimensional (2D) modeling capabilities, enabling users to simulate both vertical and horizontal contaminant migration within complex subsurface environments. This provides a more realistic…
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MIGRATEv10 Core Features: Advanced 2D Contaminant Transport Modeling
Understanding contaminant migration in complex subsurface environments requires tools that go beyond simplified assumptions. MIGRATEv10 is designed to meet this need by providing robust, two-dimensional modeling capabilities that capture the spatial and temporal dynamics of contaminant transport. This post highlights the core features that make MIGRATEv10 a powerful solution for landfill and groundwater impact assessments.…
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MIGRATEv10 vs POLLUTEv10: Fractured Layer with Sorption Comparison
Overview This example compares results from MIGRATEv10 and POLLUTEv10 for a fractured soil layer with sorption. This is one of the more complex transport scenarios, combining: The result is a system where contaminants can move rapidly through fractures while simultaneously being retarded and stored in the soil matrix. Model Setup Both models simulate a two-layer…
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MIGRATEv10 vs POLLUTEv10: Finite Mass Source Comparison
Overview This example compares finite mass transport results from MIGRATEv10 and POLLUTEv10. Unlike constant source cases, this scenario represents a limited contaminant inventory, where concentrations rise, peak, and then decline as the source is depleted. The key objective is to evaluate how both models predict: Model Setup Both models use identical physical conditions: This configuration…
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MIGRATEv10 vs POLLUTEv10: Pure Diffusion Comparison
Overview In this example, we compare pure diffusion results generated using MIGRATEv10 and POLLUTEv10 under identical conditions. The objective is to verify consistency between the two models and highlight key differences in their capabilities. Both simulations consider contaminant transport through a 4 m thick layer under pure diffusion (no advection), with constant concentration boundary conditions…

