Physical Address
304 North Cardinal St.
Dorchester Center, MA 02124
Physical Address
304 North Cardinal St.
Dorchester Center, MA 02124
This standard practice, designated D4104/D4104M, provides a rigorous analytical framework for determining the transmissivity (T) of nonleaky confined aquifers. It is specifically designed to evaluate the overdamped (force-free) response of a well-aquifer system to an instantaneous change in water level—commonly known as a slug test. The analysis is predicated on the water level recovering to its initial static elevation in an approximate exponential manner, confirming that inertial effects are negligible.
| 🟦 Parameter / Requirement | 📏 Specification from D4104/D4104M |
|---|---|
| Target Hydrogeologic Property | Transmissivity (T) |
| Aquifer Type | Nonleaky Confined |
| Hydraulic Response Type | Overdamped (Force-Free / Exponential Recovery) |
| Stress Application | Instantaneous Change in Head (Slug) |
| Assumed Well Configuration | Fully Penetrating |
| Required Field Test Standard | Test Method D4044/D4044M |
| Significant Digits & Rounding | Practice D6026 |
The analytical procedure outlined in this practice is not a standalone field guide but is explicitly designed to interpret data collected via the procedures in Test Method D4044/D4044M. Practitioners must ensure that the field test generates a force-free response suitable for this analysis.
The analysis of the recorded head vs. time data proceeds under the assumption of a fully penetrating well. The exponential nature of the overdamped response allows for a direct analytical solution for transmissivity based on the geometry of the well and the rate of water level change.
The standard openly acknowledges its primary limitation: the mathematical model assumes a fully penetrating well. Despite this, slug tests are frequently conducted in wells that only partially penetrate the aquifer. The standard provides a specific condition under which this is acceptable—namely, when the aquifer is stratified and the horizontal hydraulic conductivity (Kh) is much greater than the vertical hydraulic conductivity (Kv). In such cases, the test provides an average transmissivity for the portion of the aquifer adjacent to the open interval or screen.
| 🎯 Well Configuration | ⚡ Validity for D4104/D4104M Analysis |
|---|---|
| Fully Penetrating | Directly applicable and assumed by the analytical procedure. |
| Partially Penetrating | Acceptable for estimate if Kh >> Kv (stratified conditions). Represents an average of the tested interval. |
It is crucial to remember that this document is a set of standardized instructions. It does not replace professional judgment or education, and all aspects of the practice may not be applicable in every hydrogeologic scenario. The user bears the responsibility for establishing appropriate safety and environmental practices.
An overdamped, or force-free, response is characterized by the water level recovering to its initial static level in an approximate exponential manner with negligible inertial effects (no oscillation). This is the fundamental requirement for applying the analytical procedure in D4104/D4104M.
Yes, this is a common application. The standard accepts the use of partially penetrating wells provided the horizontal hydraulic conductivity (Kh) is much greater than the vertical hydraulic conductivity (Kv). The resulting transmissivity value is representative of the average of the aquifer interval adjacent to the well screen.
This practice is specifically designed to be used with Test Method D4044/D4044M for field data collection. Additionally, all data must be handled according to the significant digit and rounding rules in Practice D6026.
Combining values from the SI system with values from the inch-pound system results in non-conformance with the standard. Each system must be used independently, and the reported values must state which system is being applied.