August 2015 Atacama campaign
These experimental data were obtained in August 2015, in the Atacama
desert, Chile. They have been carried out in a similar way than those described
in the paper
March et al., 2012
The soil was just prepared by removing rocks and gravels, giving an
approximately flat zone. The hearths have been managed simply by firing wood
pieces directly on the soil. Temperatures were measured with a datalogger
(Omega Multi-Input Thermometer RDXL8, accepting 8 simultaneous entries) with
thermocouples (type K, gained with inconel 600, 3 mm diameter) distributed on
the surface and inside the soil under the hearths. The location of these
thermocouples is not known a priori, because they were inserted in the soil,
at some regular distance between them. Combustion was maintained between 3 and
7 hours by adding wood regularly. Twenty-four hours later, each hearth was
excavated following the same protocol. A laser theodolite was used to measure
at discrete points the contour of the hearth (after removing ashes and
spreading some water on the soil, the heating zone appears more clearly) and
the spatial location of each thermocouple. As thermocouples are flexible rods,
it is possible that their head move a bit during the excavation: for this
reason, we roughly estimate that the accuracy of their position is about 2 mm.
There was financial support from an ECOS-Sud project
(France-Chile, 2012-2016, managed by Ramiro March and Calogero Santoro).
The different contributions to the data are as follows:
- Ramiro March performed the experiment on the site (he gathered the
wood, prepared the hearth with the thermocouples, and lit the fire,
recorded the measurements). He was assisted by Wilfredo Faundes,
Cecilia Loredo and Felipe March.
- Calogero Santoro choose the site in the Atacama desert, organized the
voyage that lasted four days (lodging and transport of people and
equipment).
- Renaud Delannay provided most of equipment, and got from funding from
the University of Rennes 1 (France).
The Excel documents contain the record of temperature at thermal sensors,
stored in the first sheet named 'Temperature'; the location of the thermal
sensors (thermocouples) and the outerlimit of the heating at the soil surface
can be found in the second sheet named 'Other data'.
These raw data have been processed by inverse method by Édouard Canot; the main
results are described in the following paper:
https://hal.archives-ouvertes.fr/hal-02078646v1
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