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<!DOCTYPE article SYSTEM "http://www.hydrol-earth-syst-sci.net/inc/hess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences</journal_title>
		<journal_url>www.hydrol-earth-syst-sci.net</journal_url>
		<issn>1027-5606</issn>
		<eissn>1607-7938</eissn>
		<volume_number>6</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/hess-6-949-2002</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/6/949/2002/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/6/949/2002/hess-6-949-2002.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/6/949/2002/hess-6-949-2002.pdf</fulltext_pdf>
	<start_page>949</start_page>
	<end_page>955</end_page>
	<publication_date>0000-00-00</publication_date>
	<article_title content_type="html">Technical Note:&lt;br&gt;Practical considerations on the use of down-sized time-domain reflectometry (TDR) probes</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>M. A. Mojid</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Irrigation and Water Management, Bangladesh Agricultural University, Mymensingh – 2202, Bangladesh</affiliation>
		<affiliation numeration="2" content_type="html">E-mail: m.mojid@fz-juelich.de</affiliation>
	</affiliations>
	<abstract content_type="html">Nine time-domain
reflectometry (TDR) probes, 2 to 10 cm long, were evaluated by comparing their
measurement accuracy of TDR-pulse travel time in a sand and sandy loam soil, and
electrical conductivity in NaCl solutions. TDR probes &amp;lt;2.5 cm in length
generated trough-haped TDR waveforms with rounded corners at the points of the
pulse reflection from the probe ends. The sharpness of the pulse reflection on
the waveforms increased with both the increasing probe length and soil-water
content. The transition time for the propagation of TDR pulse at the probe
entrance increased as the soil dried up. The increased transition time caused a
rightward movement of the first peak of the waveform at the probe entrance.
Because of such peak movement, TDR-support software algorithm determined travel
path of TDR pulse through the probe that was smaller than the actual travel
path. TDR-measured pulse travel time &lt;i&gt;t&lt;/i&gt;&lt;sub&gt;TDR&lt;/sub&gt; varied erratically
with the predicted pulse travel time &lt;i&gt;t&lt;/i&gt;&lt;sub&gt;g&lt;/sub&gt; (from volumetric
soil-water content) for the probes &amp;lt;2.5 cm in length. But, for all probes
³2.5 cm in length, &lt;i&gt;t&lt;/i&gt;&lt;sub&gt;TDR&lt;/sub&gt; varied linearly with &lt;i&gt;t&lt;/i&gt;&lt;sub&gt;g&lt;/sub&gt;

and followed the 1:1 line. TDR could not measure &lt;i&gt;t&lt;/i&gt;&lt;sub&gt;TDR&lt;/sub&gt; &amp;lt;300
ps accurately. A minimum probe length &lt;i&gt;L&lt;/i&gt;&lt;sub&gt;min&lt;/sub&gt; and the lowest
allowable soil-water content &lt;i&gt;q&lt;/i&gt;&lt;sub&gt;min&lt;/sub&gt; that the probe can
accurately measure govern this lowest pulse travel time &lt;i&gt;t&lt;/i&gt;&lt;sub&gt;min&lt;/sub&gt;.
The mean absolute deviation between &lt;i&gt;t&lt;/i&gt;&lt;sub&gt;TDR&lt;/sub&gt; and &lt;i&gt;t&lt;/i&gt;&lt;sub&gt;g&lt;/sub&gt;

was 77 ps for the 2.3 cm long probe and 1.39 ps for all probes ≥2.5 cm
in length. All probes ≥2.5 cm in length measured electrical
conductivity of salt solutions s&lt;sub&gt;TDR &lt;/sub&gt;that compared well with the
electrical conductivity measured by a conductivity meter s&lt;sub&gt;m&lt;/sub&gt;. The
length of the probes did not exert any noticeable influence on the accuracy of
electrical conductivity measurement.&lt;/p&gt;
&lt;p style=&quot;line-height: 20px;&quot;&gt;&lt;b&gt;Keywords: &lt;/b&gt;TDR probe, pulse travel time, dielectric
constant, electrical conductivity&lt;/p&gt;</abstract>
	<references>
	</references>
</article>

