Category: Mining


Molly Hogan

Pressed slings

Some Jurstictions or job standards require pressed slings however I was never disappointed with any Molly Hogan I made and  we used  slip a little haywire through the dead horse part of it and then wrap it around with pliers tight and then put electrician’s tape over it. 

We used it as  well for the overshot particularly. But it wasn’t deep holes.

Some drillers would cut the seventh strand out for the unlikely event  in case the tube stuck somehow and a release wasn’t working it would fail there at the overshot connection rather than ruin or break cable.

You could make a knot joining broken cable ends by adding  two Hogan’s one inside the other  then pulling them into a kind of reef, by squashing the reef with the hydraulic head it secured it.

KDG

Preview

Water dynamics in oil production.

Drill Baby Drill

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Subsurface Hydrocarbon Extraction and Water Table Mechanics

Extracting hydrocarbons from geological formations alters the localized pressure, volume, and hydraulic equilibrium of surrounding aquifer systems. When oil is pumped from deep target reservoirs, the artificial drop in pore pressure creates a hydraulic head differential, drawing formation waters—and occasionally freshwater from shallower aquifers—downward or laterally to fill the newly created void space. In shallow unconfined aquifers or near-surface spills, the structural interaction depends strictly on phase boundaries and relative densities. Because light non-aqueous phase liquids (LNAPLs, or crude fractions lighter than water) possess a specific gravity less than 1.0, they float atop the saturated zone, resting directly on the capillary fringe above the water table. UNSATURATED ZONE (Vadose Zone)~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ [ Oil Layer / LNAPL ] <– Floats on water table (Density < 1.0)============================================================= <– Water Table [ Shallow Fresh Aquifer ] <– Displaced downward by oil head————————————————————- [ Aquitard / Confining Layer ]~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ [ Deep Saline Formation ] <– Moves upward as oil pressure drops

1. Density Dynamics & Displacement Mechanics

The physical interaction between subsurface oil and water is governed by density, capillary forces, and fluid immiscibility: * Floating Dynamics (LNAPL): Hydrocarbons with specific gravities below water (0.7 to 0.95\text{ g/cm}^3) will float. However, the oil layer exerts a downward vertical force (LNAPL head). This creates a depression in the water table directly beneath the hydrocarbon pool, displacing pure groundwater sideways and downward until capillary resistance and buoyant forces balance the weight of the oil column. * Sinking Dynamics (DNAPL): Heavy crude components, chlorinated solvents, or dense refine byproducts with specific gravities greater than 1.0 sink directly through the water table, migrating downward until they hit an impermeable aquitard layer at the base of the aquifer. * Volumetric Displacement during Extraction: As oil is removed from deep porous media, the void space must be occupied. In primary recovery, expanding formation water moves in to replace the oil. In secondary recovery, operators actively inject produced water or fresh surface water (waterflooding) to push residual oil toward production wellbores, permanently altering regional subsurface fluid distributions

.2. Worldwide Results & Global Projections|

Impact Scope | Observed & Estimated Effects | Projections ||—|—|—|| Land Subsidence | Extraction-driven pore pressure drops have led to ground compaction and surface sinking (e.g., Houston-Galveston basin lost over 3 feet of elevation historically; California’s San Joaquin Valley experienced widespread aquifer compaction). | Coastal oil-producing regions face compound flooding risks as land compaction accelerates alongside sea-level rise. || Aquifer Depletion via Injection | Worldwide, oil recovery operations inject billions of barrels of freshwater annually into deep formations to maintain field pressure. | In arid energy basins (e.g., Permian Basin, Middle East), energy-sector freshwater draw competes directly with agricultural groundwater reserves. || Inter-Aquifer Cross-Contamination | Casing failures or legacy unsealed wells create artificial conduits connecting deep saline brine formations to shallow freshwater tables. | Legacy extraction zones face rising risks of brine and hydrocarbon migration into domestic water supplies as well integrity degrades over decades. |

3. Emerging Projections & Forward Mechanics

1. The Carbon Storage

“Water Squeeze”As massive depleted oil fields transition into carbon capture and storage (CCS) reservoirs, injecting super-critical \text{CO}_2 under high pressure reverses the historical extraction flow. The injected gas displaces deep residual saline waters, potentially forcing hyper-saline plumes upward into shallow freshwater aquifers through dormant geological faults.

2. Induced Seismicity & Hydraulic Realignment

Massive injection of produced water into deep disposal wells alters effective stress along sub-surface faults. The resulting micro-seismic activity creates new fracture networks, permanently changing regional hydrogeological pathways and allowing deep formation fluids to cross into previously isolated freshwater tables.

3. Aquifer “Resurging” Post-Depletion

When mature oil fields reach the end of their production life and pumps are decommissioned, natural regional hydraulic heads begin to re-pressurize the depleted zones. This fluid resurgence can force residual hydrocarbons and volatile organic compounds upward into shallow water tables that were protected during active production by continuous extraction drawdown.

Geophysical data

Contributed:

A fascinating, foundational piece of how resource management and public science work. The short answer is **yes, absolutely**—a vast amount of geophysical data and mineral exploration information eventually makes its way into government hands and becomes a public resource.The mechanism behind how private exploration data becomes a public asset comes down to a mix of legal mandates, tax structures, and industry regulations.Here is exactly how that data lifecycle works:

## 1. The “Assessment Work” Mandate

In Canada, subsurface mineral rights are largely owned by the Crown (managed by provincial and territorial governments). When a mining or exploration company stakes a mineral claim, they don’t own the land outright; they hold the exclusive right to explore it.To keep that claim valid year after year, the company must prove they are actually doing work. They do this by submitting detailed technical reports to the provincial government (such as the Ministry of Energy, Mines and Low Carbon Innovation in BC). These are called **Assessment Reports**. * **What’s included:** Raw geophysical survey data (airborne magnetics, radiometrics, gravity), geochemical sampling results, geological maps, and drill hole logs.

* **The Confidentiality Buffer:**

To protect the company’s competitive edge while they spend money on the ground, the government keeps this data confidential for a limited time (typically 1 to 3 years, depending on the jurisdiction). * **The Public Release:** Once that confidentiality window expires, the government publishes the reports. Anyone—from a competitor to an academic researcher—can access them for free.## 2. Public Repositories & Geoscience ToolsOnce the data is released, provincial and federal geological surveys compile, standardize, and map it.

* **Geoscience Data Repositories:**

Federal bodies like the **Geological Survey of Canada (GSC)** maintain vast databases like the *Geoscience Data Repository for Geophysical Data*, which holds data from over 1,100 major surveys.

* **Digital Core Libraries:**

Governments even step in to preserve physical data. For instance, initiatives like the **Canadian Digital Core Library** are actively digitizing and scanning millions of meters of physical drill cores stored in government warehouses so the data can be analyzed using advanced computing and AI.## 3. Stock Exchange Disclosures (NI 43-101)Information also enters the public domain through financial regulations. Publicly traded exploration companies must comply with strict disclosure rules, such as

**National Instrument 43-101 (NI 43-101)**.

When a company makes a discovery, finds promising geophysical anomalies, or updates its resource estimates, it is legally required to file a comprehensive technical report on **SEDAR+**. These reports are completely public and contain heavy technical and geophysical data to ensure investors aren’t being misled.

### The Big Picture Strategy

This system creates a continuous loop. The government uses the data handed over by mining companies to update its regional geological maps. They then provide these highly detailed, large-scale baseline maps *back* to the public for free.This de-risks early-stage exploration, ensuring that a company doesn’t spend millions re-flying a geophysical survey over ground that was already thoroughly mapped decades prior. It turns private commercial data into a permanent national scientific archive.