20191219_DML_METHODS_UPDATE: Methods missing record type about sead_change_control

[visead]

Update tbl_methods.record_type_id as follows (taken from sead_staging_tng)

method_id	biblio_id	date_updated	description	method_abbrev_or_alt_name	method_group_id	method_name	record_type_id	unit_id
74		2013-04-08 12:29:53.216862+00	Measurement of total phosphate content through citric acid extraction and photospectrometer	citPtot	2	Total phosphates citric acid	12
94		2013-04-08 12:30:07.673027+00	Amount of phosphates. Standard method using HCL instead of citric acid.	P°HCL	2	Phosphate degrees HCL	12
32		2012-09-21 16:51:47.967181+00	An evaluation of the proportion of organic matter present in a sample, measured by comparing pre-burnt and post-burnt sample weights. Standard method:	LOI	2	Loss on ignition	12
33		2012-09-21 16:51:47.967181+00	A measurement of the ability of a sample to retain an induced magnetic field.	MS	2	Magnetic susceptibility	12
35		2012-09-21 16:51:47.967181+00	A measurement of the ability of a sample to retain a low frequency induced magnetic field.	MS-lo	2	Magnetic susceptibility (Low frequency)	12
36		2012-09-21 16:51:47.967181+00	A measurement of the ability of a sample to retain a high frequency induced magnetic field.	MS-hi	2	Magnetic susceptibility (High frequency)	12
38		2012-09-21 16:51:47.967181+00	Accelerator Mass Spectrometer Carbon-14 dating.	C14 AMS	3	C14 Accelerator dating	19
39		2012-09-21 16:51:47.967181+00	Conventional Carbon-14 dating.	C14	3	C14 Conventional	19
37		2012-09-21 16:51:47.967181+00	Amount of phosphates. Standard method: Inorganic phosphate content. Extraction by citric acid (2%). Based on Arrhenius and further developed by EAL. The amount of phosphate is specified as mg P2O5/100g dry soil.	P°	2	Phosphate degrees	12
106		2013-05-13 09:29:56.070308+00	Bartington MS2 & MS2D	2	MS loop	12
151		2014-04-17 05:56:03.101+00	Conventional Carbon-14 dating. Uncalibrated dates.	C14 Std	3	C14 Conventional	19	7
97		2012-12-19 13:17:57.905393+00	Soil horizon classification according to strict International Soil Reference and Information Center (ISRIC) guidelines. http://www.isric.org/isric/webdocs/docs/ISRIC_TechPap19.pdf	ISRIC horizons	18	ISRIC soil horizons	11
100		2012-12-19 13:25:50.185307+00	Soil horizon calssification according to Goldberg & Macphail (2006) Practical and theoretical geoarchaeology. Variation and simplification of ISRIC system.	Goldberg & Macphail horizons	18	Goldberg & Macphail soil horizons	11
98		2012-12-19 13:23:47.320504+00	Soil horizon classification according to strict Food and Argriculture Organization of the United Nations (FAO) guidelines. ftp://ftp.fao.org/agl/agll/docs/guidel_soil_descr.pdf and http://www.fao.org/docrep/W8594E/w8594e0g.htm for more detailed descriptions.	FAO horizons	18	FAO soil horizons	11
101		2012-12-19 14:20:49.611005+00	Soil horizons given without any specified classification system.	Undefined system horizons	18	Soil horizons by undefined system	11
154		2014-07-04 14:24:52.417266+00	Argon39-Argon 40 radiometric dating	Ar39-Ar40	3	Argon39-Argon40	19
127		2014-04-17 05:56:03.101+00	Age determined by comparison of pollen flora with reference data. A number of standard regional pollen zones have been determined through the compilation and zonation of multiple pollen profiles. Zonation is general achieved through the identification of significant changes in fauna (e.g. from birch to pine dominated), either manually or through cluster analysis.	PollenZone	19	Pollen Zonation	19	7
128		2014-04-17 05:56:03.101+00	Age determined by comparison of pollen flora with reference data. A number of standard regional pollen zones have been determined through the compilation and zonation of multiple pollen profiles. Zonation is general achieved through the identification of significant changes in fauna (e.g. from birch to pine dominated), either manually or through cluster analysis.	ArchPerCal	19	Archaeological period calendar years	19	8
129		2014-04-17 05:56:03.101+00	Age determined to an archaeological period defined in 14C years. This is a bulk method for numerous techniques for assigning a deposit to a particular cultural period, where the period boundaries have been defined by radiocarbon dating. More specific method details should preferably be given as to how the date has been derived, but may not be available.	ArchPerC14	19	Archaeological period C14 years	19	7
130		2014-04-17 05:56:03.101+00	Age determined to historical period. More specific method details should preferably be given as to how the date has been derived, but may not be available.	HistPer	19	Historical Period	19	8
131		2014-04-17 05:56:03.101+00	Age determined to geological period defined in calendar years. More specific method details should preferably be given as to how the date has been derived, but may not be available.	GeolPerCal	19	Geological calendar period	19	8
132		2014-04-17 05:56:03.101+00	Age determined to geological period defined in C14 years. More specific method details should preferably be given as to how the date has been derived, but may not be available.	GeolPerC14	19	Geological C14 period	19	7
133		2014-04-17 05:56:03.101+00	Age determined to geological period defined by radiometric methods but not necessarily radiocarbon (e.g. U-series). More specific method details should preferably be given as to how the date has been derived, but may not be available.	GeolPerRadio	19	Geological radiometric period	19	15
134		2014-04-17 05:56:03.101+00	Dating through strategraphic association, placing the sediment (and enclosed artefacts) in the context of geological layers of known or unknown age.	Strat(Geol)	19	Stratigraphic (Geological)	19	15
135		2014-04-17 05:56:03.101+00	Dating by relation to volcanic ash layer of a known calendar age.	TephraCal	20	Tephrochronology Calendar	19	8
136		2014-04-17 05:56:03.101+00	Dating by relation to volcanic ash layer dated by radiocarbon.	TephraC14	20	Tephrochronology C14	19	7
137		2014-04-17 05:56:03.101+00	Dating by artefact typology with calendar date. The form, design and material of an artefact may allow it to be placed in the context of a known sequence of artefact characteristics (a typological sequence). This allows it to be dated through the assumption that the typologies are correctly and independently dated. There is a slight danger or circular reasoning is the constraints of independent dating are not rigourously enforced, and a tendency for typologies to persist even if evidence suggests that there may be problems.	TypoCal	19	Artefact typology (calendar years)	19	8
138		2014-04-17 05:56:03.101+00	Dating by artefact typology with radiometric date. The form, design and material of an artefact may allow it to be placed in the context of a known sequence of artefact characteristics (a typological sequence). This allows it to be dated through the assumption that the typologies are correctly and independently dated. There is a slight danger or circular reasoning is the constraints of independent dating are not rigourously enforced, and a tendency for typologies to persist even if evidence suggests that there may be problems.	TypoRadio	19	Artefact typology (radiometric years)	19	15
139		2014-04-17 05:56:03.101+00	Unspecified dating method leading to an archaeological date in calendar years.	ArchCal	20	Other archaeological dating	19	8
140		2014-04-17 05:56:03.101+00	A sequence of radiocarbon dates may be compared with variation in the C14 calibration curve, and dates nudged so that they align with the curve. The method requires a sequence to be tightly dated and may be especially useful around flatter parts of the calibration curve. User discretion is required.	Wiggle	20	Wiggle matching of 14C dates	19	8
141		2014-04-17 05:56:03.101+00	Dating method which relies on the predictable growth pattern of some lichen species. Some lichens (e.g. Rhizocarpon geographicum) exhibit colonisation, linear growth and non-linear phases of growth. By calibrating sizes against surfaces of known age (e.g. buildings, grave stones) it is possible to guage the age of exposure of a surface through the sizes of the lichens growing on it. A number of variations exist in terms of how to measure. The method has been applied to historical and archaeological remains as well as to geological features such as erosion surfaces and raised beaches.	Lichen	20	Lichenometry	19	8
142		2014-04-17 05:56:03.101+00	Calendar years derived by unknown or unspecified method.	UnknownCal	20	Calendar date by unknown method	19	8
143		2014-04-17 05:56:03.101+00	Derivation of calendar date by reference to  geological processes, features or events (e.g. volcanic eruption, earthquake).	GeolCal	20	Geologically derived calendar date	19	8
144		2014-04-17 05:56:03.101+00	Dating based on historical documentation.	HistCal	20	Historical Records	19	8
145		2014-04-17 05:56:03.101+00	Unspecified dating method.	UnknownOther	21	Other date by unknown method	19	15
146		2014-04-17 05:56:03.101+00	U234/U238	3	U-Series U234/U238	19	15
147		2014-04-17 05:56:03.101+00	U-Series	3	Uranium-Series (general)	19	15
148		2014-04-17 05:56:03.101+00	Dating by a radiocarbon method, the details of which are not provided in the publication or supporting material.	C14 Unspec.	3	Radiocarbon (14C Unspecified)	19	7
149		2014-04-17 05:56:03.101+00	Dating by an unspecified radiometric method (information missing in publication).	UnknownRadio	3	Radiometric date by unknown method	19	7
152		2014-04-17 05:56:03.101+00	Age determination based on the post-mortem decay (or racemization/epimerization) of amino acids in fossils. The method has primarily been used to date shells, and less sucessfully on bone, teeth and wood under some conditions.	AAR	3	Amino Acid Racemization	19	15
153		2014-04-17 05:56:03.101+00	Age determination by radiocarbon on humic substances extracted by pretreatment of sediments (e.g. peat, colluvium). A number of method variations are applied, aimed at dating different fractions of the sample (as opposed to the bulk dating of organic matter), including: humic acid fraction (alkali soluble) and humin fraction (alkali insoluble). Modern dates are generally determined through AMS, but older dates may have been aquired through standard counting.	C14 Humous	3	C14 dating of humic substances in sediment	19	7
155		2014-07-13 22:00:00+00	Period based dating method leading to a range of potential archaeological dates in unspecified years.	ArchPer	20	Archaeological period (unspecified)	19	15
156		2018-05-02 12:13:47.999285+00	Age determined to geological period using undefined (or possibly multiple) method(s).	GeolPer	19	Geological period (unspecified)	19
150		2014-04-17 05:56:03.101+00	Dating using the release of stored energy properties of (mainly sonte) material previously exposed to the sun.	TL	22	Thermoluminescence	19	15
159		2019-11-03 12:16:24.809745+00	Calendar years date provided by the calibration of a radiocarbon age. Exact dating method unspecified.	Cal	20	Calibrated radiocarbon date (method unspecified)	19	8
163		2019-11-03 12:16:24.809745+00	Calendar years date provided by calibration of an AMS radiocarbon age.	CalAMS	20	Calibrated AMS radiocarbon date	19	8

[visead]

All nulls should be set to Unknown record type

[roger-mahler]

Resolved in 20191219_DML_METHODS_UPDATE