Electromagnetic Depth Soundings:
10.------------------------, 10.------------------------. N ::IE ~ w ~ '" "'0.1 \~ 0 M z SIDE VIEW PLAN VIEW 0.01 LI --'---'---LLL-'---LLLlI ~-L---"---LLL..ll..L.LJ'-':';;' 0.01 1 100 10 100 fr Fig. 1. The behavior of the magnetic and elect...
Gespeichert in:
| Hauptverfasser: | , , , |
|---|---|
| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Boston, MA
Springer US
1967
|
| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | 10.------------------------, 10.------------------------. N ::IE ~ w ~ '" "'0.1 \~ 0 M z SIDE VIEW PLAN VIEW 0.01 LI --'---'---LLL-'---LLLlI ~-L---"---LLL..ll..L.LJ'-':';;' 0.01 1 100 10 100 fr Fig. 1. The behavior of the magnetic and electric fields from a vertical magnetic dipole source at the surface of the earth (after Wait [1951,1955]). earth, the experimental curve so plotted should have the same shape as a portion of the ap propriate theoretical curve, but with the ordinates and abscissas shifted by an amount dependent on the resistivity. The conductivity can be determined from the amount of shift between the field data and the theoretical curve. A detailed description of the curve matching procedure is found in a text by Keller and Frischknecht (1966). The curve matching procedure, though used, has several disadvantages. Measurements must be made over a diagnostic portion of the theoretical curve, one in which there is some curvature, so that the amount of shift required to make a match can be determined uniquely. This means that the approximate conductivity of the earth must be known when measurements are made. Secondly, determination of a single value of conductivity requires measurements made over a wide range of frequencies. This would appear to be wasteful of data, inasmuch as the equations indicate that a single measurement at a single frequency should be enough to de termine conductivity |
| Beschreibung: | 1 Online-Ressource (VIII, 316 p) |
| ISBN: | 9781468406702 |
| DOI: | 10.1007/978-1-4684-0670-2 |
Internformat
MARC
| LEADER | 00000nmm a2200000zc 4500 | ||
|---|---|---|---|
| 001 | BV045176585 | ||
| 003 | DE-604 | ||
| 005 | 00000000000000.0 | ||
| 007 | cr|uuu---uuuuu | ||
| 008 | 180911s1967 |||| o||u| ||||||eng d | ||
| 020 | |a 9781468406702 |9 978-1-4684-0670-2 | ||
| 024 | 7 | |a 10.1007/978-1-4684-0670-2 |2 doi | |
| 035 | |a (ZDB-2-EES)978-1-4684-0670-2 | ||
| 035 | |a (OCoLC)1053810967 | ||
| 035 | |a (DE-599)BVBBV045176585 | ||
| 040 | |a DE-604 |b ger |e aacr | ||
| 041 | 0 | |a eng | |
| 049 | |a DE-634 | ||
| 082 | 0 | |a 526.1 |2 23 | |
| 082 | 0 | |a 550 |2 23 | |
| 100 | 1 | |a Vanyan, L. L. |e Verfasser |4 aut | |
| 245 | 1 | 0 | |a Electromagnetic Depth Soundings |c by L. L. Vanyan, L. Z. Bobrovnikov, V. M. Davidov, A. N. Kuznetsov, V. L. Loshenitzina, G. M. Morozova, A. I. Shtimmer, E. I. Terekhin |
| 264 | 1 | |a Boston, MA |b Springer US |c 1967 | |
| 300 | |a 1 Online-Ressource (VIII, 316 p) | ||
| 336 | |b txt |2 rdacontent | ||
| 337 | |b c |2 rdamedia | ||
| 338 | |b cr |2 rdacarrier | ||
| 520 | |a 10.------------------------, 10.------------------------. N ::IE ~ w ~ '" "'0.1 \~ 0 M z SIDE VIEW PLAN VIEW 0.01 LI --'---'---LLL-'---LLLlI ~-L---"---LLL..ll..L.LJ'-':';;' 0.01 1 100 10 100 fr Fig. 1. The behavior of the magnetic and electric fields from a vertical magnetic dipole source at the surface of the earth (after Wait [1951,1955]). earth, the experimental curve so plotted should have the same shape as a portion of the ap propriate theoretical curve, but with the ordinates and abscissas shifted by an amount dependent on the resistivity. The conductivity can be determined from the amount of shift between the field data and the theoretical curve. A detailed description of the curve matching procedure is found in a text by Keller and Frischknecht (1966). The curve matching procedure, though used, has several disadvantages. Measurements must be made over a diagnostic portion of the theoretical curve, one in which there is some curvature, so that the amount of shift required to make a match can be determined uniquely. This means that the approximate conductivity of the earth must be known when measurements are made. Secondly, determination of a single value of conductivity requires measurements made over a wide range of frequencies. This would appear to be wasteful of data, inasmuch as the equations indicate that a single measurement at a single frequency should be enough to de termine conductivity | ||
| 650 | 4 | |a Earth Sciences | |
| 650 | 4 | |a Geophysics/Geodesy | |
| 650 | 4 | |a Earth sciences | |
| 650 | 4 | |a Geophysics | |
| 700 | 1 | |a Bobrovnikov, L. Z. |4 aut | |
| 700 | 1 | |a Davidov, V. M. |4 aut | |
| 700 | 1 | |a Kuznetsov, A. N. |4 aut | |
| 776 | 0 | 8 | |i Erscheint auch als |n Druck-Ausgabe |z 9781468406726 |
| 856 | 4 | 0 | |u https://doi.org/10.1007/978-1-4684-0670-2 |x Verlag |z URL des Erstveröffentlichers |3 Volltext |
| 912 | |a ZDB-2-EES | ||
| 940 | 1 | |q ZDB-2-EES_Archiv | |
| 999 | |a oai:aleph.bib-bvb.de:BVB01-030565815 | ||
| 966 | e | |u https://doi.org/10.1007/978-1-4684-0670-2 |l BTU01 |p ZDB-2-EES |q ZDB-2-EES_Archiv |x Verlag |3 Volltext | |
Datensatz im Suchindex
| _version_ | 1804178864450043904 |
|---|---|
| any_adam_object | |
| author | Vanyan, L. L. Bobrovnikov, L. Z. Davidov, V. M. Kuznetsov, A. N. |
| author_facet | Vanyan, L. L. Bobrovnikov, L. Z. Davidov, V. M. Kuznetsov, A. N. |
| author_role | aut aut aut aut |
| author_sort | Vanyan, L. L. |
| author_variant | l l v ll llv l z b lz lzb v m d vm vmd a n k an ank |
| building | Verbundindex |
| bvnumber | BV045176585 |
| collection | ZDB-2-EES |
| ctrlnum | (ZDB-2-EES)978-1-4684-0670-2 (OCoLC)1053810967 (DE-599)BVBBV045176585 |
| dewey-full | 526.1 550 |
| dewey-hundreds | 500 - Natural sciences and mathematics |
| dewey-ones | 526 - Mathematical geography 550 - Earth sciences |
| dewey-raw | 526.1 550 |
| dewey-search | 526.1 550 |
| dewey-sort | 3526.1 |
| dewey-tens | 520 - Astronomy and allied sciences 550 - Earth sciences |
| discipline | Physik Geologie / Paläontologie |
| doi_str_mv | 10.1007/978-1-4684-0670-2 |
| format | Electronic eBook |
| fullrecord | <?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>03011nmm a2200457zc 4500</leader><controlfield tag="001">BV045176585</controlfield><controlfield tag="003">DE-604</controlfield><controlfield tag="005">00000000000000.0</controlfield><controlfield tag="007">cr|uuu---uuuuu</controlfield><controlfield tag="008">180911s1967 |||| o||u| ||||||eng d</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9781468406702</subfield><subfield code="9">978-1-4684-0670-2</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-1-4684-0670-2</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ZDB-2-EES)978-1-4684-0670-2</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)1053810967</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)BVBBV045176585</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-604</subfield><subfield code="b">ger</subfield><subfield code="e">aacr</subfield></datafield><datafield tag="041" ind1="0" ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="049" ind1=" " ind2=" "><subfield code="a">DE-634</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">526.1</subfield><subfield code="2">23</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">550</subfield><subfield code="2">23</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Vanyan, L. L.</subfield><subfield code="e">Verfasser</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Electromagnetic Depth Soundings</subfield><subfield code="c">by L. L. Vanyan, L. Z. Bobrovnikov, V. M. Davidov, A. N. Kuznetsov, V. L. Loshenitzina, G. M. Morozova, A. I. Shtimmer, E. I. Terekhin</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Boston, MA</subfield><subfield code="b">Springer US</subfield><subfield code="c">1967</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (VIII, 316 p)</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">10.------------------------, 10.------------------------. N ::IE ~ w ~ '" "'0.1 \~ 0 M z SIDE VIEW PLAN VIEW 0.01 LI --'---'---LLL-'---LLLlI ~-L---"---LLL..ll..L.LJ'-':';;' 0.01 1 100 10 100 fr Fig. 1. The behavior of the magnetic and electric fields from a vertical magnetic dipole source at the surface of the earth (after Wait [1951,1955]). earth, the experimental curve so plotted should have the same shape as a portion of the ap propriate theoretical curve, but with the ordinates and abscissas shifted by an amount dependent on the resistivity. The conductivity can be determined from the amount of shift between the field data and the theoretical curve. A detailed description of the curve matching procedure is found in a text by Keller and Frischknecht (1966). The curve matching procedure, though used, has several disadvantages. Measurements must be made over a diagnostic portion of the theoretical curve, one in which there is some curvature, so that the amount of shift required to make a match can be determined uniquely. This means that the approximate conductivity of the earth must be known when measurements are made. Secondly, determination of a single value of conductivity requires measurements made over a wide range of frequencies. This would appear to be wasteful of data, inasmuch as the equations indicate that a single measurement at a single frequency should be enough to de termine conductivity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geophysics/Geodesy</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geophysics</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bobrovnikov, L. Z.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Davidov, V. M.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kuznetsov, A. N.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="776" ind1="0" ind2="8"><subfield code="i">Erscheint auch als</subfield><subfield code="n">Druck-Ausgabe</subfield><subfield code="z">9781468406726</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1007/978-1-4684-0670-2</subfield><subfield code="x">Verlag</subfield><subfield code="z">URL des Erstveröffentlichers</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-2-EES</subfield></datafield><datafield tag="940" ind1="1" ind2=" "><subfield code="q">ZDB-2-EES_Archiv</subfield></datafield><datafield tag="999" ind1=" " ind2=" "><subfield code="a">oai:aleph.bib-bvb.de:BVB01-030565815</subfield></datafield><datafield tag="966" ind1="e" ind2=" "><subfield code="u">https://doi.org/10.1007/978-1-4684-0670-2</subfield><subfield code="l">BTU01</subfield><subfield code="p">ZDB-2-EES</subfield><subfield code="q">ZDB-2-EES_Archiv</subfield><subfield code="x">Verlag</subfield><subfield code="3">Volltext</subfield></datafield></record></collection> |
| id | DE-604.BV045176585 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:45Z |
| institution | BVB |
| isbn | 9781468406702 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030565815 |
| oclc_num | 1053810967 |
| open_access_boolean | |
| owner | DE-634 |
| owner_facet | DE-634 |
| physical | 1 Online-Ressource (VIII, 316 p) |
| psigel | ZDB-2-EES ZDB-2-EES_Archiv ZDB-2-EES ZDB-2-EES_Archiv |
| publishDate | 1967 |
| publishDateSearch | 1967 |
| publishDateSort | 1967 |
| publisher | Springer US |
| record_format | marc |
| spelling | Vanyan, L. L. Verfasser aut Electromagnetic Depth Soundings by L. L. Vanyan, L. Z. Bobrovnikov, V. M. Davidov, A. N. Kuznetsov, V. L. Loshenitzina, G. M. Morozova, A. I. Shtimmer, E. I. Terekhin Boston, MA Springer US 1967 1 Online-Ressource (VIII, 316 p) txt rdacontent c rdamedia cr rdacarrier 10.------------------------, 10.------------------------. N ::IE ~ w ~ '" "'0.1 \~ 0 M z SIDE VIEW PLAN VIEW 0.01 LI --'---'---LLL-'---LLLlI ~-L---"---LLL..ll..L.LJ'-':';;' 0.01 1 100 10 100 fr Fig. 1. The behavior of the magnetic and electric fields from a vertical magnetic dipole source at the surface of the earth (after Wait [1951,1955]). earth, the experimental curve so plotted should have the same shape as a portion of the ap propriate theoretical curve, but with the ordinates and abscissas shifted by an amount dependent on the resistivity. The conductivity can be determined from the amount of shift between the field data and the theoretical curve. A detailed description of the curve matching procedure is found in a text by Keller and Frischknecht (1966). The curve matching procedure, though used, has several disadvantages. Measurements must be made over a diagnostic portion of the theoretical curve, one in which there is some curvature, so that the amount of shift required to make a match can be determined uniquely. This means that the approximate conductivity of the earth must be known when measurements are made. Secondly, determination of a single value of conductivity requires measurements made over a wide range of frequencies. This would appear to be wasteful of data, inasmuch as the equations indicate that a single measurement at a single frequency should be enough to de termine conductivity Earth Sciences Geophysics/Geodesy Earth sciences Geophysics Bobrovnikov, L. Z. aut Davidov, V. M. aut Kuznetsov, A. N. aut Erscheint auch als Druck-Ausgabe 9781468406726 https://doi.org/10.1007/978-1-4684-0670-2 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | Vanyan, L. L. Bobrovnikov, L. Z. Davidov, V. M. Kuznetsov, A. N. Electromagnetic Depth Soundings Earth Sciences Geophysics/Geodesy Earth sciences Geophysics |
| title | Electromagnetic Depth Soundings |
| title_auth | Electromagnetic Depth Soundings |
| title_exact_search | Electromagnetic Depth Soundings |
| title_full | Electromagnetic Depth Soundings by L. L. Vanyan, L. Z. Bobrovnikov, V. M. Davidov, A. N. Kuznetsov, V. L. Loshenitzina, G. M. Morozova, A. I. Shtimmer, E. I. Terekhin |
| title_fullStr | Electromagnetic Depth Soundings by L. L. Vanyan, L. Z. Bobrovnikov, V. M. Davidov, A. N. Kuznetsov, V. L. Loshenitzina, G. M. Morozova, A. I. Shtimmer, E. I. Terekhin |
| title_full_unstemmed | Electromagnetic Depth Soundings by L. L. Vanyan, L. Z. Bobrovnikov, V. M. Davidov, A. N. Kuznetsov, V. L. Loshenitzina, G. M. Morozova, A. I. Shtimmer, E. I. Terekhin |
| title_short | Electromagnetic Depth Soundings |
| title_sort | electromagnetic depth soundings |
| topic | Earth Sciences Geophysics/Geodesy Earth sciences Geophysics |
| topic_facet | Earth Sciences Geophysics/Geodesy Earth sciences Geophysics |
| url | https://doi.org/10.1007/978-1-4684-0670-2 |
| work_keys_str_mv | AT vanyanll electromagneticdepthsoundings AT bobrovnikovlz electromagneticdepthsoundings AT davidovvm electromagneticdepthsoundings AT kuznetsovan electromagneticdepthsoundings |