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https://issues.apache.org/jira/browse/TIKA-1532?page=com.atlassian.jira.plugin.system.issuetabpanels:comment-tabpanel&focusedCommentId=14520968#comment-14520968
]
Chris A. Mattmann commented on TIKA-1532:
-----------------------------------------
Good to go, committing!
{noformat}
[INFO] ------------------------------------------------------------------------
[INFO] BUILD SUCCESS
[INFO] ------------------------------------------------------------------------
[INFO] Total time: 57.451 s
[INFO] Finished at: 2015-04-29T23:30:04-07:00
[INFO] Final Memory: 90M/1640M
[INFO] ------------------------------------------------------------------------
[chipotle:~/tmp/tika] mattmann% ls
46.patch LICENSE.txt pom.xml tika-bundle/
tika-java7/ tika-server/
CHANGES.txt NOTICE.txt target/ tika-core/
tika-parent/ tika-translate/
HEADER.txt README.md tika-app/ tika-dotnet/
tika-parsers/ tika-xmp/
KEYS assembly.xml tika-batch/ tika-example/
tika-serialization/
[chipotle:~/tmp/tika] mattmann% svn status
? 46.patch
M CHANGES.txt
? tika-batch/target
A tika-core/src/main/java/org/apache/tika/sax/DIFContentHandler.java
M tika-core/src/main/resources/org/apache/tika/mime/tika-mimetypes.xml
M tika-core/src/test/java/org/apache/tika/TikaDetectionTest.java
M tika-core/src/test/java/org/apache/tika/mime/MimeDetectionTest.java
A tika-parsers/src/main/java/org/apache/tika/parser/dif
A
tika-parsers/src/main/java/org/apache/tika/parser/dif/DIFContentHandler.java
A tika-parsers/src/main/java/org/apache/tika/parser/dif/DIFParser.java
A
tika-parsers/src/main/java/org/apache/tika/parser/xml/DIFContentHandler.java
A tika-parsers/src/main/java/org/apache/tika/parser/xml/DIFParser.java
M
tika-parsers/src/main/resources/META-INF/services/org.apache.tika.parser.Parser
A tika-parsers/src/test/java/org/apache/tika/parser/dif
A tika-parsers/src/test/java/org/apache/tika/parser/dif/DIFParserTest.java
A tika-parsers/src/test/java/org/apache/tika/parser/xml/DIFParserTest.java
A tika-parsers/src/test/resources/test-documents/Zamora2010.dif
[chipotle:~/tmp/tika] mattmann% java -jar
tika-app/target/tika-app-1.9-SNAPSHOT.jar -t
tika-parsers/src/test/resources/test-documents/Zamora2010.dif
Title: Zamora 2010 Using Sediment Geochemistry, Particle Size
Distribution and Remote Sensing to Study Provenance in the
Kronebreen/Kongsvegen Glaciers, West Spitsbergen, Svalbard
Geographic Data:
Southernmost_Latitude : 78.833
Northernmost_Latitude : 79.016
Westernmost_Longitude : 11.64
Easternmost_Longitude : 13.34
[chipotle:~/tmp/tika] mattmann% java -jar
tika-app/target/tika-app-1.9-SNAPSHOT.jar -d
tika-parsers/src/test/resources/test-documents/Zamora2010.dif
application/dif+xml
[chipotle:~/tmp/tika] mattmann%
[chipotle:~/tmp/tika] mattmann% java -jar
tika-app/target/tika-app-1.9-SNAPSHOT.jar -m
tika-parsers/src/test/resources/test-documents/Zamora2010.dif
Content-Length: 10199
Content-Type: application/dif+xml
DIF-Data_Center-Data_Center_Name-Long_Name: Advanced Cooperative Arctic Data
and Information Service
DIF-Data_Center-Data_Center_Name-Short_Name: ACADIS
DIF-Data_Center-Data_Center_URL: http://www.aoncadis.org/
DIF-Data_Center-Personnel-Contact_Address-Address: NCAR/CISL
DIF-Data_Center-Personnel-Contact_Address-Address: P.O. Box 3000
DIF-Data_Center-Personnel-Contact_Address-City: Boulder
DIF-Data_Center-Personnel-Contact_Address-Country: USA
DIF-Data_Center-Personnel-Contact_Address-Postal_Code: 80307
DIF-Data_Center-Personnel-Contact_Address-Province_or_State: CO
DIF-Data_Center-Personnel-First_Name: ACADIS
DIF-Data_Center-Personnel-Last_Name: User Services
DIF-Data_Center-Personnel-Role: DATA CENTER CONTACT
DIF-Entry_ID: 00794186-48f9-11e3-9dcb-00c0f03d5b7c
DIF-Entry_Title: Zamora 2010 Using Sediment Geochemistry, Particle Size
Distribution and Remote Sensing to Study Provenance in the
Kronebreen/Kongsvegen Glaciers, West Spitsbergen, Svalbard
DIF-Last_DIF_Revision_Date: 2015-02-05
DIF-Metadata_Name: ACADIS IDN DIF
DIF-Metadata_Version: 9.8.4
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Category: EARTH SCIENCE
DIF-Parameters-Term: OCEAN/LAKE RECORDS
DIF-Parameters-Term: OCEAN/LAKE RECORDS
DIF-Parameters-Term: GLACIERS/ICE SHEETS
DIF-Parameters-Term: LAND TEMPERATURE
DIF-Parameters-Term: EROSION/SEDIMENTATION
DIF-Parameters-Term: MARINE SEDIMENTS
DIF-Parameters-Term: EROSION/SEDIMENTATION
DIF-Parameters-Term: GLACIERS/ICE SHEETS
DIF-Parameters-Term: GLACIERS/ICE SHEETS
DIF-Parameters-Term: LAND RECORDS
DIF-Parameters-Term: EROSION/SEDIMENTATION
DIF-Parameters-Term: OCEAN TEMPERATURE
DIF-Parameters-Term: OCEAN/LAKE RECORDS
DIF-Parameters-Term: MARINE SEDIMENTS
DIF-Parameters-Term: EROSION/SEDIMENTATION
DIF-Parameters-Term: FROZEN GROUND
DIF-Parameters-Term: GLACIERS/ICE SHEETS
DIF-Parameters-Term: FROZEN GROUND
DIF-Parameters-Term: EROSION/SEDIMENTATION
DIF-Parameters-Term: EROSION/SEDIMENTATION
DIF-Parameters-Topic: PALEOCLIMATE
DIF-Parameters-Topic: PALEOCLIMATE
DIF-Parameters-Topic: TERRESTRIAL HYDROSPHERE
DIF-Parameters-Topic: LAND SURFACE
DIF-Parameters-Topic: LAND SURFACE
DIF-Parameters-Topic: OCEANS
DIF-Parameters-Topic: LAND SURFACE
DIF-Parameters-Topic: CRYOSPHERE
DIF-Parameters-Topic: TERRESTRIAL HYDROSPHERE
DIF-Parameters-Topic: PALEOCLIMATE
DIF-Parameters-Topic: LAND SURFACE
DIF-Parameters-Topic: OCEANS
DIF-Parameters-Topic: PALEOCLIMATE
DIF-Parameters-Topic: OCEANS
DIF-Parameters-Topic: LAND SURFACE
DIF-Parameters-Topic: CRYOSPHERE
DIF-Parameters-Topic: CRYOSPHERE
DIF-Parameters-Topic: CRYOSPHERE
DIF-Parameters-Topic: LAND SURFACE
DIF-Parameters-Topic: LAND SURFACE
DIF-Parameters-Variable_Level_1: SEDIMENTS
DIF-Parameters-Variable_Level_1: VARVE DEPOSITS
DIF-Parameters-Variable_Level_1: GLACIER MASS BALANCE/ICE SHEET MASS BALANCE
DIF-Parameters-Variable_Level_1: LAND SURFACE TEMPERATURE
DIF-Parameters-Variable_Level_1: SEDIMENTS
DIF-Parameters-Variable_Level_1: TURBIDITY
DIF-Parameters-Variable_Level_1: SEDIMENT TRANSPORT
DIF-Parameters-Variable_Level_1: GLACIER MASS BALANCE/ICE SHEET MASS BALANCE
DIF-Parameters-Variable_Level_1: GLACIERS
DIF-Parameters-Variable_Level_1: SEDIMENTS
DIF-Parameters-Variable_Level_1: SEDIMENTATION
DIF-Parameters-Variable_Level_1: WATER TEMPERATURE
DIF-Parameters-Variable_Level_1: LAKE LEVELS
DIF-Parameters-Variable_Level_1: SEDIMENT TRANSPORT
DIF-Parameters-Variable_Level_1: DEGRADATION
DIF-Parameters-Variable_Level_1: SOIL TEMPERATURE
DIF-Parameters-Variable_Level_1: GLACIERS
DIF-Parameters-Variable_Level_1: PERIGLACIAL PROCESSES
DIF-Parameters-Variable_Level_1: ENTRAINMENT
DIF-Parameters-Variable_Level_1: SUSPENDED SOLIDS
DIF-Related_URL-Description: Data Center top-level access page for this resource
DIF-Related_URL-URL:
http://www.aoncadis.org/dataset/id/00794186-48f9-11e3-9dcb-00c0f03d5b7c.html
DIF-Related_URL-URL_Content_Type-Type: GET DATA
DIF-Spatial_Coverage-Easternmost_Longitude: 13.34
DIF-Spatial_Coverage-Northernmost_Latitude: 79.016
DIF-Spatial_Coverage-Southernmost_Latitude: 78.833
DIF-Spatial_Coverage-Westernmost_Longitude: 11.64
DIF-Summary-Abstract: Abstract: Sediment provenance at the
Kronerbreen/Kongsvegen glaciers in Spitsbergen can be used to understand the
effects that climate change can have on the sedimentation in fjords, and
streams at northern latitudes. These sediments are directly related to glacial
processes and reflect the conditions under which they formed. Such conditions
are sensitive to global climate change, which is amplified in northern
latitudes, creating a unique environment for climate change research.
Quantitative provenance studies have never been carried out in the Kongsfjorden
before, and can provide data for a better understanding of glacial processes
and dynamics, and changes in erosional conditions. Particularly, sedimentation
rates and sediment grain size distribution can help unravel the glacial history
of the area. This study will focus on analyzing the grain size distribution of
the material being deposited by the mentioned glaciers and finding the source
rock of these sediments. Fine sediment was transported by streams and upflows
identified in the field, and fed by the glaciers melting ice. On the other
hand, coarser material ranging from cobble to boulder size was deposited by
ice, moraines, and alluvial processes. Sediment and rock samples were collected
during the months of July and August 2009, along the terminus of the glacier,
and in the surrounding areas, respectively. Grain size analysis was performed
on the samples using a Malvern Mastersizer with the resulting in different
groups showing a change in particle size and sorting depending on the location
along the glacier. This analysis is important as mineral composition and
transportation is influenced by grain size. Electron microprobe studies were
carried out on sediment grains to obtain a rough compositional profile of the
sediments, and a first-order mineralogical make-up. The microprobe results
provided us with information about composition of some of the minerals present,
based on the content of Fe, Ca, K and Al derived from the erosion of the local
lithologies. Chemical composition can distinguish sediments derived from
different sources, and may ultimately be compared with representative rock
samples taken from the moraines. Due to the limited accessibility to some
areas, many geological units in the Kongsfjorden area have not been mapped or
studied, limiting the possible comparisons with contributing material to the
fjord’s seafloor. Remote sensing techniques were used to map lithologies in
previously unmapped regions using ENVI®, and ASTER satellite imagery. A GER
3700 radiospectrometer was used to collect spectral properties of the rock
samples. These properties were compared to the outcrops in the satellite
imagery giving us an idea of the bedrock composition of the area. The results
of our research can be compared with future studies in order to obtain
information, regarding responses in the glacier dynamics and processes, related
to climate change.
X-Parsed-By: org.apache.tika.parser.DefaultParser
X-Parsed-By: org.apache.tika.parser.dif.DIFParser
resourceName: Zamora2010.dif
[chipotle:~/tmp/tika] mattmann%
{noformat}
> DIF Parser
> ----------
>
> Key: TIKA-1532
> URL: https://issues.apache.org/jira/browse/TIKA-1532
> Project: Tika
> Issue Type: New Feature
> Components: parser
> Reporter: Aakarsh Medleri Hire Math
> Assignee: Chris A. Mattmann
> Labels: memex
>
> MIME Type detection & content parser for .dif format
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