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Remote sensing for resources development and environmental management (Volume 2)

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CC BY: Attribution 4.0 International. You can find more information here.

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fullscreen: Remote sensing for resources development and environmental management (Volume 2)

Multivolume work

Persistent identifier:
856342815
Title:
Remote sensing for resources development and environmental management
Sub title:
proceedings of the 7th international Symposium, Enschede, 25 - 29 August 1986
Year of publication:
1986
Place of publication:
Rotterdam
Boston
Publisher of the original:
A. A. Balkema
Identifier (digital):
856342815
Language:
English
Additional Notes:
Volume 1-3 erschienen von 1986-1988
Editor:
Damen, M. C. J.
Document type:
Multivolume work

Volume

Persistent identifier:
856641294
Title:
Remote sensing for resources development and environmental management
Sub title:
proceedings of the 7th international Symposium, Enschede, 25 - 29 August 1986
Scope:
IX Seiten, Seiten 551-956
Year of publication:
1986
Place of publication:
Rotterdam
Boston
Publisher of the original:
A,. A. Balkema
Identifier (digital):
856641294
Illustration:
Illustrationen, Diagramme
Signature of the source:
ZS 312(26,7,2)
Language:
English
Usage licence:
Attribution 4.0 International (CC BY 4.0)
Editor:
Damen, M. C. J.
Editor:
International Society for Photogrammetry and Remote Sensing, Commission of Photographic and Remote Sensing Data
Publisher of the digital copy:
Technische Informationsbibliothek Hannover
Place of publication of the digital copy:
Hannover
Year of publication of the original:
2016
Document type:
Volume
Collection:
Earth sciences

Chapter

Title:
6 Hydrology: Surface water, oceanography, coastal zone, ice and snow. Chairman: K. A. Ulbricht, Co-chairman: Mikio Takagi, Liaison: R. Spanhoff
Write comment:
Wegen zu enger Bindung kommt es teilweise im Original zu Textverlust.
Document type:
Multivolume work
Structure type:
Chapter

Chapter

Title:
Rainlog and preslog: Novel tools for in-situ measurements. D. de Hoop
Document type:
Multivolume work
Structure type:
Chapter

Contents

Table of contents

  • Remote sensing for resources development and environmental management
  • Remote sensing for resources development and environmental management (Volume 2)
  • Cover
  • Title page
  • Title page
  • Title page
  • Table of contents
  • 5 Non-renewable resources: Geology, geomorphology and engineering projects. Chairman: J. V. Taranik, Liaison: B. N. Koopmans
  • 6 Hydrology: Surface water, oceanography, coastal zone, ice and snow. Chairman: K. A. Ulbricht, Co-chairman: Mikio Takagi, Liaison: R. Spanhoff
  • A methodology for integrating satellite imagery and field observations for hydrological régionalisation in Alpine catchments. R. Allewijn
  • The JRC program for marine coastal monitoring. J. A. Bekkering
  • Shape and variability of the absorption spectrum of aquatic humus. H. Buiteveld & F. de Jong, R. Spanhoff, M. Donze
  • Rainlog and preslog: Novel tools for in-situ measurements. D. de Hoop
  • Simple classifiers of satellite data for hydrologic modelling. R. S.Drayton, T. R. E. Chidley & W. C. Collins
  • The delineation and classification of inland wetlands utilizing fcir stereo imagery. Stephen A. Estrin
  • A hydrological comparison of Landsat TM, Landsat MSS and black & white aerial photography. M. J. France & P. D. Hedges
  • Application of remote sensing in hydromorphology for third world development: A resource development study in parts of Haryana (India). A. S. Jadhav
  • Remote sensing of flow characteristics of the strait of Öresund. L. Jönsson
  • Present state, changes and quality of Sologne and Brenne, two French large wetlands, studied with the MSS and TM Landsat data. Michel Lenco, Jean-Pierre Dedieu
  • The quantification of floodplain inundation by the use of LANDSAT and Metric Camera information, Belize, Central America. S. T. Miller
  • Remote sensing as a tool for assessing environmental effects of hydroelectric development in a remote river basin. W. Murray Paterson & Stewart K. Sears
  • Environmental assessment for large scale civil engineering projects with data of DTM and remote sensing. Taichi Oshima & Atsushi Rikimaru, Youichi Kato & Masaharu Nakamura
  • Sea surface temperature studies in Norwegian coastal areas using AVHRR- and TM thermal infrared data. J. P. Pedersen
  • Satellite data in aquatic area research: Some ideas for future studies. Jouko T. Raitala
  • Analysis of Landsat multispectral-multitemporal images for geologic-lithologic map of the Bangladesh Delta. A. Sesören
  • Water quality monitoring of Lake Balaton using LANDSAT MSS data. H. Shimoda, M. Etaya & T. Sakata, L. Goda & K. Stelczer
  • Determination of spectral signatures of natural water by optical airborne and shipbome instruments. D. Spitzer & M. R. Wernand
  • Classification of bottom composition and bathymetry of shallow waters by passive remote sensing. D. Spitzer & R. W. J. Dirks
  • Satellite remote sensing of the coastal environment of Bombay. V. Subramanyan
  • A study with NOAA-7 AVHRR-imagery in monitoring ephemeral streams in the lower catchment area of the Tana River, Kenya. J. W. van den Brink
  • A simple atmospheric correction algorithm for Landsat Thematic Mapper satellite images. P. I. G. M. Vanouplines
  • 7 Human settlements: Urban surveys, human settlement analysis and archaeology. Chairman: W. G. Collins, Co-chairman: B. C. Forster, Liaison: P. Hofstee
  • 8 Geo-information systems. Chairman: J. J. Nossin
  • Cover

Full text

Symposium on Remote Sensing for Resources Development and Environmental Management / Enschede / August 1986 
707 
Rainlog and preslog: Novel tools for in-situ measurements 
D.de Hoop 
International Institute for Aerospace Survey and Earth Sciences (ITC), Enschede, Netherlands 
1. INTRODUCTION 
The rainlog and preslog electronic water level log 
gers were developed at the International Institute 
for Aerospace Survey and Earth Sciences (ITC), 
Enschede, and after some redesigning, are produced 
by Siemens Netherlands, The Hague. 
The instruments measure and record water pressure 
over long periods (for example, at sixty minutes 
intervals for a period of 12 months) without requir 
ing maintenance or changing of batteries. Expensive 
test stations are not required. The loggers, togeth 
er with the data-processing facilities, provide a 
new scientific approach to field measurements. 
The pressure recordings ar.e controlled by a micro 
processor and are stored in a removable internal 
memory block (the "Eprom"). The capacity of the 
Eprom is 10240 records. The records are read by a 
personal computer (Epson, type PX-8) with an "Eprom 
reader". Depending on the software chosen the re 
sults can be presented raw or in calculated form. 
Two types of loggers are available; both have the 
same electronics. The difference is based on the 
type of sensor used. Rainlog has a relative pressure 
sensor; preslog has an absolute pressure sensor. The 
standard range for rainlog is 2 meters. The standard 
range for preslog is 0 to 4 bar, which at sea level 
is equivelent to a range of 30 meters. 
The precision of the measurements is approximately 
0.2 percent for preslog and 0.5 percent for rainlog. 
The resolution is 2000 for the rainlog and 4000 for 
the 4 bar-type preslog. The measuring interval can 
be set between 30 seconds and 60 minutes (60 minutes 
is standard). A built-in audio signal provides an 
operational check. 
The loggers were designed for both accuracy and 
durability. Durability requires permanent attachment 
to the internal panel of all parts except the remov 
able memory block (Eprom) and also very firm place 
ment of the panel in the steel cylinder. Opening the 
cylinder to replace the Eprom or to re-set the re 
cording interval requires a vise, which is usually 
not available at a test site. We therefore recommend 
transporting the entire logger to a field office 
where the necessary equipment can be kept and where 
there is less danger of damage to the Eprom. 
1.1 Preslog applications 
River level 
To record river levels, a logger must be anchored 
in the riverbed. After installation, it is left for 
a maximum period of 12 months. The instrument func 
tions without disturbance, despite shifting bottom 
sand and gravel. After the operating period, the 
logger must be retrieved and opened; the memory 
block is removed and read by the personel computer. 
An additional "dry" preslog is required for barome 
tric correction. One dry logger covers an extensive 
area and thus can be combined with several wet 
loggers. 
Groundwater level 
Preslog can also function as a groundwater level 
logger. Its three inch diameter allows placement in 
waterpipes for pump-test. Data from several tests 
can be recorded in sequence by placing a "marker" 
in the recorded data to indicate the end of one 
test and the beginning of the next. 
1.2 Rainlog applications 
To record rainfall, a rainlog is connected to the 
bottom of a rain collection container. Only in 
creases in pressure are recorded. Decreases in 
pressure caused by evaporation or emptying the 
container are ignored. A simple program later shows 
the results of a year's data collection.
	        

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