05.11.2012 Views

Geophysical Survey in Archaeological Field Evaluation - HELM

Geophysical Survey in Archaeological Field Evaluation - HELM

Geophysical Survey in Archaeological Field Evaluation - HELM

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

4<br />

2.2 <strong>Field</strong>work<br />

All fieldwork should be conducted under the<br />

pr<strong>in</strong>ciple of repeatability; <strong>in</strong> other words, that,<br />

with<strong>in</strong> reason, the data obta<strong>in</strong>ed should be<br />

capable of <strong>in</strong>dependent duplication. <strong>Field</strong>workers<br />

must ensure that every effort is made on<br />

site to be courteous and considerate <strong>in</strong> their<br />

deal<strong>in</strong>gs with landowners, local residents and<br />

organisations, respect<strong>in</strong>g all aspects of the<br />

environment. A high level of professionalism<br />

is necessary at all times.<br />

Correct observance should be made of any<br />

legal constra<strong>in</strong>ts on site – for <strong>in</strong>stance, the<br />

requirement of a Section 42 Licence for<br />

survey over scheduled monuments and<br />

other protected places, and the licence now<br />

needed for survey on National Trust land<br />

(Part II, 7.3).<br />

2.2.1 The survey grid<br />

This is the network of control po<strong>in</strong>ts used to<br />

locate the geophysical survey measurements<br />

relative to base mapp<strong>in</strong>g and/or absolute position<br />

on the Earth’s surface, (see Part IV, 1.1). Whether<br />

physically marked on the ground or measured<br />

while survey<strong>in</strong>g us<strong>in</strong>g a global position<strong>in</strong>g<br />

system (GPS), these must be located to<br />

survey-grade accuracy (±0.1m). The survey<br />

grid must be <strong>in</strong>dependently re-locatable on<br />

the ground by a third party, by measurement<br />

to local permanent features, and/or by the use<br />

of GPS coord<strong>in</strong>ates. All locational <strong>in</strong>formation<br />

must be geo-referenced. In certa<strong>in</strong> cases (eg<br />

where permanent features are absent), and with<br />

appropriate permission, it may be acceptable to<br />

emplace permanent survey markers.<br />

Care must be taken to ensure that any survey<br />

markers or other equipment are not a hazard<br />

to people or animals.<br />

2.2.2 Magnetometer survey<br />

<strong>Survey</strong> must be conducted with a cont<strong>in</strong>uously<br />

record<strong>in</strong>g magnetometer of appropriate<br />

sensitivity.<br />

Area survey must be the preferred method<br />

of ground coverage <strong>in</strong> all <strong>in</strong>stances where this<br />

is practicable.<br />

The maximum acceptable sampl<strong>in</strong>g <strong>in</strong>terval<br />

for an area survey is 0.25m on traverses a<br />

maximum of 1m apart.<br />

Magnetometer scann<strong>in</strong>g, as a method of <strong>in</strong>itially<br />

assess<strong>in</strong>g the magnetic response of a site, may<br />

be used at the discretion of surveyors who<br />

are experienced <strong>in</strong> its application, for devis<strong>in</strong>g<br />

(or advis<strong>in</strong>g upon) an appropriate evaluation<br />

strategy that will use other methods. The<br />

technique should not otherwise be <strong>in</strong>cluded<br />

<strong>in</strong> briefs or specifications.<br />

2.2.3 Earth resistance: area survey<br />

The maximum acceptable sampl<strong>in</strong>g <strong>in</strong>terval for<br />

area surveys is 1m along traverses separated<br />

by a maximum of 1m.<br />

Area surveys, us<strong>in</strong>g the tw<strong>in</strong> probe (or tw<strong>in</strong><br />

electrode) probe configuration, are the preferred<br />

method of ground coverage. The square array<br />

(often employed on cart-based systems) is also<br />

acceptable for area surveys. Other methods<br />

require special justification.<br />

For tw<strong>in</strong> probe systems the mobile probe<br />

spac<strong>in</strong>g should usually be 0.5m; wider<br />

separations and/or multiplexed arrays require<br />

explanation. The equivalent spac<strong>in</strong>g for a<br />

square array would typically be 0.75m.<br />

2.2.4 Ground penetrat<strong>in</strong>g radar survey<br />

Generally, this technique will be applied for<br />

the detailed <strong>in</strong>vestigation of a site by <strong>in</strong>dividual<br />

profiles and the visualisation of the data as<br />

time slices. A maximum traverse spac<strong>in</strong>g of<br />

0.5m is recommended with samples taken<br />

at <strong>in</strong>tervals of 0.05m.<br />

Specific site conditions and the aims of the<br />

survey may require an alternative sampl<strong>in</strong>g<br />

methodology to be adopted, but this must<br />

be fully justified <strong>in</strong> any support<strong>in</strong>g<br />

specification documents.<br />

Determ<strong>in</strong>ation of an appropriate sampl<strong>in</strong>g<br />

<strong>in</strong>terval, centre frequency of antenna(s) used<br />

and sub-surface velocities used for depth<br />

estimation from the result<strong>in</strong>g data must be<br />

supported through an appropriate survey<br />

design, <strong>in</strong>clud<strong>in</strong>g field test measurements<br />

where appropriate.<br />

2.2.5 Magnetic susceptibility survey<br />

Magnetic susceptibility survey should not take<br />

precedence over magnetometer survey where<br />

the latter is practicable.<br />

Areas of high topsoil magnetic susceptibility<br />

should be complemented by detailed area<br />

magnetometer survey. Some areas of low<br />

or <strong>in</strong>different magnetic susceptibility values<br />

should also be sampled with detailed<br />

magnetometer coverage, to confirm that<br />

under the prevail<strong>in</strong>g site conditions, changes<br />

<strong>in</strong> magnetic susceptibility do correlate with<br />

archaeological potential.<br />

The chosen method(s) of magnetic susceptibility<br />

measurement must be appropriate to prevail<strong>in</strong>g<br />

ground surface conditions.<br />

Measurements of topsoil magnetic susceptibility,<br />

for area surveys and transects, must be made<br />

at <strong>in</strong>tervals not exceed<strong>in</strong>g 10m.<br />

Where possible, such topsoil measurements<br />

must be compared and contrasted with<br />

those obta<strong>in</strong>ed from subsoil and local<br />

archaeological features.<br />

2.3 Data treatment<br />

Area surveys must be conducted, and<br />

subsequent data treated, so as to result<br />

<strong>in</strong> a data-set that is as uniform as possible.<br />

Edge-effects between contiguous survey<br />

areas should be m<strong>in</strong>imised.<br />

A copy of unprocessed raw data must be<br />

reta<strong>in</strong>ed and archived (see below, 6 Archiv<strong>in</strong>g).<br />

Raw data collected <strong>in</strong> the field must be of high<br />

quality. Any data-collection artefacts subsequently<br />

apparent <strong>in</strong> the survey data should be identified<br />

and removed us<strong>in</strong>g appropriate data process<strong>in</strong>g<br />

(Part IV, 2.1). All such process<strong>in</strong>g should be<br />

clearly described. Any data collection artefacts<br />

that cannot be corrected by data process<strong>in</strong>g<br />

should be described and clearly dist<strong>in</strong>guished<br />

from possible archaeological anomalies.<br />

If data has been seriously compromised dur<strong>in</strong>g<br />

collection, a return to the site to re-survey<br />

the affected area(s) should be considered.<br />

2.4 Data <strong>in</strong>terpretation<br />

The <strong>in</strong>terpretation of survey data must be<br />

undertaken by a competent archaeological<br />

geophysicist who is knowledgeable of the<br />

archaeological and geomorphological conditions<br />

prevail<strong>in</strong>g on site. Consultation must also take<br />

place with other site specialists (eg landscape<br />

archaeologists, aerial photographers) wherever<br />

possible.<br />

The <strong>in</strong>terpretation of magnetometer and<br />

magnetic susceptibility data must endeavour to<br />

dist<strong>in</strong>guish anthropogenic from other causes of<br />

magnetic enhancement on the site(s) concerned.<br />

A clear dist<strong>in</strong>ction must always be made<br />

between <strong>in</strong>terpretation that is scientifically<br />

demonstrable, and <strong>in</strong>terpretation based on<br />

<strong>in</strong>formed speculation.<br />

Any reference to ‘negative evidence’ must be<br />

fully qualified and expla<strong>in</strong>ed. Lack of geophysical<br />

anomalies cannot be taken to imply a lack of<br />

archaeological features, and <strong>in</strong> such cases an<br />

alternative evaluation procedure – eg trial<br />

trench<strong>in</strong>g, or the use of a different geophysical<br />

technique – should be considered.<br />

2.5 The survey report<br />

All fieldwork must be followed by a report.<br />

This will be a clear and succ<strong>in</strong>ct text, supported<br />

by tables, figures, appendices and references as<br />

necessary (see below, 2.5.1). It ought to stand<br />

<strong>in</strong>dependent of support<strong>in</strong>g material and should<br />

comb<strong>in</strong>e the qualities of concise technical

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!