#SoilAndCulture: #ethnopedology and science. Can the soil be seen as an
artifact?    
What are the implications
between  a cultural landscape and  the soil local knowledge in  other cultures?
by Marta Laureanti
I
started  to ask myself if  the soil could be considered as an artifact.
What is the perception of the soil in contemporary cultures? Does exist   soil local  knowledge? In which way we could have
different approach to the recording strategy if we consider other categories of
knowledge, other instruments?
Some ethnopedological
researches  gave me new inputs for my
questions. Ethnopedology is
the study of local knowledge about soils and their management, and in recent
times it  has been increasingly
recognized for its contribution to the evaluation of land use in relation to
soil quality and sustainable agriculture. It covers a wide diversity of topics:
the formalization of local soil and land knowledge into classification
schemes,  the comparison of local and
technical soil classifications, the analysis of local land evaluation systems,
and the assessment of agro-ecological management practices (Barrera-Bassols,
 Zick, 2003).
As many studies  in different part of the world have
demonstrated, in some cultures can be identified    local
knowledge  of the soil properties, often
based on qualitative characteristics of the soils: colours, stoniness, taste,
consistence (Bautista,Zinck, 2010; Wells & Mihok , 2004;
 Ali, 2003; Barrera- Bassols , Zinck, Van Ranst, 2006; VanDerwarker, 2005;
 Gray, Morant, 2003; Ryder, 2003; Wells & Mihok , 2004;
 Saito,Linquist,Keobulapha,Shiraiwa,Horie, 2006; Adderley, Simpson,Kirscht,
 Adam,Spencer,Sanderson, 2004).
For example  The Maya soil classification (MSC) is a
natural system based on key properties, such as relief position, rock types,
size and quantity of stones, color of topsoil and subsoil, depth, water
dynamics, and plant-supporting processes. The MSC addresses the soil properties
of surficial and subsurficial horizons, and uses plant communities as qualifier
in some cases. It was demonstrated that the MSC was  more accurate than the WRB (World Reference
Base for Soil Resources) for classifying Leptosols (Bautista,Zinck,
 2010).
Such studies  could suggest to the archaeologists that a
quantitative research  isn’t  the only way to collect the data. Integrated
approaches can allow more points of view and perspectives. 
A topographical research in Netherland
has suggested that ancient names of portion of land showed a soil/land management
practices often governed by the biophysical position of the farms. On the
higher sandy areas soil fertility was a major constraint for sustainable
farming, whereas on the lower, clayey regions soil workability and water
management were important issues. The farmers applied their local knowledge of
the soil/land systems consistently and in a holistic manner (Siderius, De Bakker, 2003).
Another example is
constituted by the farmers of Damarpota in Bangladesh, which distinguish soil
types primarily on the basis of color, consistence, texture, organic matter
content, drainage, salinity, acidity, and fertility . They use indigenous
methods such as visual observation while tilling, tasting by tongue, feeling
and rubbing with fingers to determine various soil properties. Despite their lack of knowledge of soil
genesis and chemistry, it was observed that  the farmers are highly knowledgeable in various
soil properties that affect crop cultivation (Ali, 2003). 
Among some Mesoamerican community soil colour plays  an important role in the recognition of soil
distribution patterns by farmers. In general, farmers relate soil colour to
elevation, slope gradient, vegetation and relief. Dark soils occur on high
elevations, forestland and valleys. Yellowish soils occur on slopes and in
plains, while reddish soils occur on washed steep slopes and in low-elevation
valleys  (Barrera-Bassols,Zinck,Van Ranst, 2006).
What I am trying to say is that some scientific categories, such  the only use of chemical analysis on the soil
doesn’t reflect the same level of knowledge that local inhabitants could have
by using other categories, and the same properties that they see could be not
represented by technical analysis. 
Some studies  were led on artificial mounds. 
 Colored soils seemed deliberately selected and deposited to create distinct
patterns of color (Sherwood & Kidder, 2011; Bernardini, 2004;
 Johansen, 2004; Owoc, 2004; Papadopoulos, Bejko, Morris, 2008; Saunders, 2004). Besides excavations at Neolithic settlement
sites in Orkney have observed varied uses of cultural sediments (traditionally
referred to under the blanket term midden) as being incorporated into site
construction (Cluett, 2007).
Another example comes from the Mediterrean area. A  study  led  at 84 temple of
classical mainland Greece, several Aegean islands and Cyprus on bedrock geology topographic
setting, compass orientation, soil profile and plant cover has revealed a
striking patterns  between the soil and
vegetation  and the dedication to
particular deities and cults (Retallack, 2008).
In an integrated research
led by archaeologists  and anthropologist
at Mexican town of Cuentepec, it was demonstrated that studying
only the chemical characterization of the soils in some house  at this village did not capture the whole
spectrum of activities recorded by the direct observations of behavior of the locals inhabitats. Translating this results on the archaeological
research, this
disjuncture prompted them to rethink human spatial behavior and the ways in
which chemical and residue data were analyzed and interpreted by
archaeologists. They realized that using multiple
chemical elements simultaneously to identify discrete spatial areas raised the
analytic ability to identify unique combinations or suites of chemical elements
in space(fig.3). This could provide
clues to the way space was socially used and structured (Dore, Lopez Varela, 2010).
Fig. 3 Display of the chemical data in color
after spatial analysis in one house in Cuantupec, Mexico (Dore, Lopez
 Varela, 2010)
ML
 
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