The invention relates generally to a portable ground thawing system and method for placing shovel test pits (STPs) in frozen ground.
Prior to developing a tract of land, it is sometimes required to make an archaeological survey to determine whether the planned development might negatively impact ancient cultural remains, buried artifacts or other generally hidden objects of historical value.
A shovel test pit (STP) is a standard method for performing an initial assessment phase of an archaeological survey. In many cases, shovel testing strategies are designed to identify archaeological resources and to delineate their boundaries. Within a specified project area, a series of small test holes are dug by hand using a shovel (typically) in order to determine whether the soil contains cultural remains. A hand shovel is used due to its relative gentleness and finesse compared to chipping or hacking with an axe pick, or other forms of aggressive digging. Artifacts buried in the soil are less likely to be damaged using a hand shoveling technique, through which haptic feedback can inform a trained technician of conditions as they are encountered. Soil excavated from the STP is sifted or screened through a wire mesh to determine whether any relevant artifacts are contained in the soil. The collected results of STP findings can be mapped over the project area to determine whether further archaeological investigation is necessary.
The depth of an STP depends on the depth at which either the bedrock or the sterile subsoil is found. Occasionally the excavation of shovel test pits (STPs) into frozen ground becomes necessary. Frozen ground presents at least two very serious obstacles to excavating STPs. First, digging in frozen earth can be very labor intensive and time consuming. Second, frozen earth tends to remain in large clods that are resistant to sifting and screening through wire mesh. For these reasons, it is generally disfavored to excavate STPs in frozen ground. This reluctance to perform STPs in freezing conditions can result in development delays for many months.
The project area over which STPs must be placed is often remote and/or rugged undeveloped terrain which must be traversed by foot or with the aid of off-road vehicles like four-wheelers. In Northern climates during the winter months, snowmobiles may be the only effective means of transport. As a result of these often-difficult conditions, all equipment used to perform STP survey must be easily packable and transportable by foot, four-wheeler, or snowmobile. Large and/or heavy equipment is simply impractical for performing STPs, especially during the winter months in Northern climates.
Moreover, State Historic Preservation Office standards, as well as guidelines established by other agencies, typically prohibit or discourage archaeological investigations in frozen ground, during times when the ground is snow covered, or when it is snowing or raining heavily. For this reason, the industry has avoided the development of solutions designed for winter field conditions.
There is therefore a need in the art to facilitate the placement of STPs in frozen ground using equipment that is easy to transport.
According to a first aspect of the invention, a portable ground thawing system comprises a heat chamber having an open bottom surrounded by a sidewall and a closed top. A charging inlet is disposed in the sidewall. An exhaust flue is disposed in the sidewall. A heater has a discharge nozzle configured to emit a stream of hot gas along a discharge vector. The heater is disposed proximate to the heat chamber with the discharge vector passing through the charging inlet. The flue is located generally opposite the charging inlet.
According to a second aspect of the invention, a method is provided for excavating a Shovel Test Pit (STP) in frozen ground. The method comprises the steps of: preparing a test area by clearing debris and removing snow accumulations above a threshold limit, placing the open bottom of a heat chamber on the test area, orienting the heat chamber so that its charging inlet is leeward and its exhaust flue is windward relative to the prevailing wind direction, directing a stream of hot gas from a heater along a discharge vector passing through the charging inlet, and circulating hot gases through a heat loft within the heat chamber above the charging inlet prior to exiting through the flue.
The system and method of this invention enable in-season soil conditions, i.e., not frozen ground, to be easily replicated for taking geological samples and any other expedient purposes. The invention thaws earthy sediments to the point that they could be removed from the ground by standard shovel testing operation and subsequently passed through a mesh during a typical screen operation. The system and method are effective, at least in part, by controlling heated gas so as to flow consistently across the frozen ground surface below the heat chamber. As a result, the invention enables winter-time near-surface archaeological testing to be conducted during urgent or emergency situations, such as buried utility repair, or to conduct further investigations surrounding the inadvertent find of human remains. This invention offers a solution to the prevailing local standards and guidelines that typically discourage archaeological investigations in frozen ground.
These and other features and advantages of the present invention will become more readily appreciated when considered in connection with the following detailed description and appended drawings, wherein:
Referring to the figures, wherein like numerals indicate like or corresponding parts throughout the several views, a portable ground thawing system is generally shown in one exemplary embodiment for use in placing shovel test pits (STPs) and such other applications as may be found expedient to excavate small portions of earth during the winter months in Northern climates.
The portable ground thawing system includes a heat chamber, generally indicated at 10. The heat chamber 10 is a hollow construction having an open bottom 12 surrounded by a sidewall 14 and a closed top 16. The sidewall 14 can be made of steel or other suitable heat-compatible material. In the illustrated examples the heat chamber 10 takes the form of a generally cylindrical volume in which case the sidewall 14 is generally cylindrical and the top 16 is generally circular and the bottom 12 is also generally circular. It has been discovered that a commercial grade steel drum of 30-gallon size will suffice for construction of the heat chamber 10. However, the heat chamber 10 can take many different shapes and forms, including cube-like, dome-like, pyramid-like and cone-like to name a few. Naturally, other (non-cylindrical) forms of the heat chamber 10 will dictate corresponding adaptations to the shapes of the bottom 12, top 16 and sidewall 14 features. In all contemplated variations, the open bottom 12 end is posited to face the underlying ground surface.
At least one handle 18 is attached to the heat chamber 10 to facilitate handling. It has been found expedient to attached two such handles 18 adjacent the top 16, diametrically located opposite one another on the sidewall 14. The handles 18 can be economically fabricated from a section of metallic rod bent to form a D-shaped loop that is welded or otherwise affixed directly to the heat chamber 10. A thermal resistant metal can be used, if desired, to reduce the risk of burn injury to the operators. The loop configuration shown in the drawing is advantageous for naturally shedding heat so as to reduce the risk of burn injury when the system is in operation. Of course, handles 18 of other numbers, shapes and mounted locations can be substituted for those illustrated in the figures if desired.
A charging inlet 20 disposed in the sidewall 14. The charging inlet 20 has an upper extremity 22 and a lower extremity 24. The lower extremity 24 of the charging inlet 20 is axially spaced from bottom 12 by a lower extremity distance IL. The charging inlet 20 is shown to have a generally rectangular shape throughout the accompanying illustrations, however other shapes are certainly possible, including but not limited to circular. Regardless of shape, the charging inlet 20 will have upper 22 and lower 24 extremities. In one example, the charging inlet 20 is an opening approximately 8-inches high by 12-inches wide.
Particularly beneficial results have been achieved when the upper extremity 22 of the charging inlet 20 is axially spaced generally midway between the bottom 12 and the top 16 of the heat chamber 10. More specifically, the upper extremity 22 is preferably located within ±10% of the midline between the bottom 12 and the top 16 of the heat chamber 10. Thus, in the example of a heat chamber 10 having an overall height of 30 inches (i.e., axial distance between top 16 and bottom 12), the midline will fall at 15 inches as measured from either end 12, 16. Thus, ±10% equal 3 inches on either side of the midline. In other words, in this example the upper extremity 22 will preferably fall between about 12 inches and 18 inches as measured from the bottom 12.
In use, the heat chamber 10 is positioned so that the charging inlet 20 is located on the leeward side relative to the wind direction W. By maintaining the upper extremity 22 of the charging inlet 20 within 10% of the midline, a substantial volume of upwardly confined space can be established in a heat loft 25 inside the heat chamber 10. The trapped volume inside the heat chamber 10 above the upper extremity 22 is the heat loft 25, as indicated in
An exhaust flue 26 is disposed in the sidewall 14 to emit excess gas from the heat chamber 10. The flue 26 is located generally opposite the charging inlet 20. Thus, in examples where the heat chamber 10 is cylindrical, the flue 26 can be seen as diametrically opposed to the charging inlet 20. In use, the heat chamber 10 is positioned so that the exhaust flue 26 is located on the windward side relative to the wind direction W.
The flue 26 has a first edge 28 adjacent the bottom 12 and a second edge 30 adjacent the top 16. The first edge 28 of the flue 26 is axially spaced from bottom 12 by a first flue distance F1, whereas the second edge 30 is axially spaced from bottom 12 by a second flue distance F2. In practice, a first flue distance F1 of approximately 4 inches has been found to provide satisfactory results. The second flue distance F2 is less than or equal to the lower extremity distance IL of the charging inlet 20 on the opposite side of the heat chamber 10. That is to say, the lower extremity 24 of the charging inlet 20 may be configured so as not to extend as low as the exhaust flue 26. As a result, cooler gas will be more effectively forced to exit the heat chamber 10 below the level of the charging inlet 20.
In the illustrated examples, the flue 26 is generally rectangular, with the first 28 and second 30 edges being parallel to one another and extending horizontally relative to the ground. In practice, a flue 26 having a size of 6-inches high by 8-inches wide has been found effective. However, the flue 26 can take many different shapes. In some contemplated embodiments, the flue is circular or oval. In some contemplated embodiments, the flue is louvered.
In the illustrated examples, a baffle 32 is moveably connected to the flue 26. The baffle 32, best seen in
Furthermore, a moveable interface 36 can be incorporated to support the baffle 32 for movement relative to the flue 26. The moveable interface 36 is shown in one exemplary form in
Those of skill in the art will readily appreciate alternative designs by which to achieve a moveable interface 36. In one contemplated embodiment, relative sliding movement between baffle 32 and flue 26 is achieved by seating a suitably configured baffle in external tracks affixed to the sidewall 14 above and below the flue 26. In this example, the tracks are open at each end enabling the baffle 32 to be removed, inverted, then re-installed in the tracks. In another contemplated embodiment, the baffle 32 is rotatably attached relative to the flue 26 with features enabling both redirection of exhaust (via directional fin 34) and alteration of the flue 26 exhaust area. In still other contemplated embodiments, the baffle 32 can be mechanized to effect directionality and restrictions much like the vent controls found in passenger cars and other HVAC applications. Indeed, many alternative designs are possible and within the scope of the person having ordinary skill in this art.
The ground thawing system further includes a portable heater, generally indicated at 40 in
A mounting base supports the heater 40 at an incline so that the discharge vector V passes through the charging inlet 20 in a downward trajectory. The mounting base can be any of several forms, including bi-pod and tripod arrangements, as well as mechanically adjustable tilt tables. In the illustrated examples, however, the mounting base is depicted in the basic but effective form of a generally flat sub-base 44 combined with a plurality of shims 46. The shims 46 serve as easily adjustable props when disposed between the sub-base 44 and the heater 40 to achieve the desired downward trajectory of the discharge vector V. Simplicity is favored in view of the need to transport the components of the system over harsh terrain during cold weather as well as avoiding unnecessary mechanical function that would be subject to freezing and inoperability.
To supply electrical power to the heater 40, an electricity generator 48 is provided with appropriate electrical extension cord. A fuel source 50 is also provided for supplying suitable combustible fuel to the heater 40. In
The method of using the system to thaw frozen ground will now be described. In particular, a novel cold weather method is provided for replicating in-season soil conditions, i.e., not frozen ground, such that sediments are thawed to the point they can be removed from the ground by standard shovel testing operation (no chipping or hacking) and pass through mesh of specified size during typical screen operation. In one example, the mesh size is approximately 0.635-centimeter (0.25-inch).
A designated test area 52 (
In some cases, it may be desirable to leave a threshold limit of snow on the ground. In practice, a threshold limit of 4-6 inches has been found satisfactory. Leaving a thin layer of snow on the test site 52 may help reduce the risk of biomass ignition and the melt-water expedites the thawing process. Also, the heat chamber 10 will eventually sink toward the ground, helping to seal any gaps created by an uneven ground surface. In operation, additional snow can be shoveled around the bottom 12 of the heat chamber 10, if desired, to maintain a seal due to uneven ground features and produce additional melt-water.
A suitably rated heater 40 is placed on mounting base supports 44, 46 so as to direct hot gas into the charging inlet 20 along a downward discharge vector V. The nozzle of the heater 40 is preferably positioned about 2 to 3 inches from the charging inlet 20. Operative connections are made between the heater 40 and its sources 48, 50 of electricity and fuel.
To commence the thawing operation, the heater 40 is ignited so as to force a jet stream of hot gas through the charging inlet 20 at a downward angle V that is also pointing in the upwind direction. By reference to
Considering the desire to avoid blow-back, one might incorrectly assume that the heat chamber 10 should be rotated on the test area 52 so that its charging inlet 20 is pointing windward and its flue 26 is leeward relative to the wind direction W—i.e., opposite to that described in this present method. Logic would seem to indicate (incorrectly as it turns out) that if the charging inlet 20 is pointed windward, that wind pressure would assist in preventing blow-back and even help in evacuating exhaust gasses through the flue 26. However, the present invention defies natural logic by orienting the inlet 20 and flue 26 features as previously specified. The novel arrangement of elevated charging inlet 20 relative to flue 26 combined with a downwardly directed discharge vector V produces a powerful and effective natural swirling flow of gasses within the heat chamber 10. The induced currents are sufficiently powerful to overcome the pressure of the wind W, such that the wind pressure can be exploited to supplement the effects of the baffle 32. That is to say, the wind W provides (to the degree available) additional back-pressure against the escaping gases, thus enabling the operator more control over temperature stabilization inside the heat chamber 10. Additionally, wind W blowing into the rear of the heater 40 can produce negative operating effects.
As previously mentioned, a relatively large heat loft 25 established inside the heat chamber 10 above the charging inlet 20 performs beneficial radiant and convective functions. As a radiant heat body, the heat loft 25 continuously projects heat energy through the open bottom 12 onto the exposed ground surface. Convectively, internal currents circulating through the heat loft 25 recharge with high heat energy before circulating across the ground surface. Thus, the intentionally induced swirling gas flow as indicated in
By manipulating the baffle 32 via the moveable interface 36, the internal currents can be adjusted and altered in relation to ambient conditions to maintain the desired internal temperatures inside the heat chamber 10. If the wind W is blowing more or less strongly, or more or less consistently, the operator may wish to orient the baffle 32 to either of the inverted positions represented in
It has been found that in at least some sub-freezing climates, an STP can be completed using the method described above in approximately one hour on average replicating field-season ground conditions where ground cover was present (excluding lawn grass). In cases where lawn grass cover was present, or no ground cover was present, STPs could be completed on average in approximately three hours replicating normal field conditions. It is suspected that rather than the ground cover itself causing significant differences in time, the variance may instead be attributable to the amount of moisture present below a grassy ground surface trapped within finer, less-well-drained sediments.
Once field-season ground conditions have been replicated, the heater 40 is switched off and removed from the test area 52. The heat chamber 10 is also removed from the test area 52 with the aid of the handles 18 to avoid burn-related injury. In the thawed earth, an STP can be excavated. In some cases, a suitable STP may be hand-dug with shovel 54, as depicted in
Soil from the STP is passed through suitably sized mesh 56 to identify artifacts 58. Information about the soils observed in each STP is typically recorded in a field logbook to assist with interpretation of how the site deposits formed over time and to help evaluate whether soil disturbances have occurred. Upon completion of the STP, the excavated soil is returned to the hole and tamped down in an effort to return the test area 52 to its initial condition.
The foregoing invention has been described in accordance with the relevant legal standards, thus the description is exemplary rather than limiting in nature. Variations and modifications to the disclosed embodiment may become apparent to those skilled in the art and fall within the scope of the invention.
This application claims priority to Provisional Patent Application US 62/929,190 filed on Nov. 1, 2019, the entire disclosure of which is hereby incorporated by reference and relied upon.
Number | Date | Country | |
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62929190 | Nov 2019 | US |