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            <gco:CharacterString>Cite this dataset as: Buesseler, K. (2020) Water-column total Thorium-234 and Uranium-238 from R/V Knorr cruises KN199-04 and KN204-01 in the Subtropical northern Atlantic Ocean from 2010-2011 (U.S. GEOTRACES NAT project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2) Version Date 2013-03-25 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.3836.2 [access date]</gco:CharacterString>
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Value and uncertainty from equation derived in Owens et al. (2011)&amp;lt;br /&amp;gt;
&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp; &amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp; U-238 (dpm/L) = (Salinity * 0.0786) - 0.315&amp;lt;br /&amp;gt;
Salinity was measured onboard the ship by the Scripps Ocean Data Facility.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Thorium-234&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Determined by the widely-adopted 4 L method. Shallow (&amp;amp;lt; 1000 m) samples were collected from the SIO ODF Rosette and deep samples (&amp;amp;gt;1000 m) were collected from Niskin bottles hung above in situ pumps. Data are decay corrected to the mid-point time between when bottles 1 and 12 were fired for shallow casts and when the messenger was dropped for deep cast. All surface samples were collected using a deck-mounted pump (denoted as bottle 13). All data have been recovery-corrected using the Th-230/Th-229 recovery method (see references below) to account for any loss of sample material during processing. All samples were analyzed using RISO Laboratory Anti-coincidence Beta Counters, using a helium/1% butane mixture. Overall method efficiency was determined by minimizing the percent difference between mean U-238 and Th-234 values for samples from &amp;amp;gt;1000 m to &amp;amp;gt; 1000 m from the bottom (44.5 % for KN 199-4 and 46.4 % for KN 204-01a and KN 204-01b).&amp;lt;/p&amp;gt;</gco:CharacterString>
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                            <gco:CharacterString>GEOTRACES is a SCOR sponsored program; and funding for program infrastructure development is provided by the U.S. National Science Foundation.
GEOTRACES gained momentum following a special symposium, S02: Biogeochemical cycling of trace elements and isotopes in the ocean and applications to constrain contemporary marine processes (GEOSECS II), at a 2003 Goldschmidt meeting convened in Japan. The GEOSECS II acronym referred to the Geochemical Ocean Section Studies To determine full water column distributions of selected trace elements and isotopes, including their concentration, chemical speciation, and physical form, along a sufficient number of sections in each ocean basin to establish the principal relationships between these distributions and with more traditional hydrographic parameters;
* To evaluate the sources, sinks, and internal cycling of these species and thereby characterize more completely the physical, chemical and biological processes regulating their distributions, and the sensitivity of these processes to global change; and
* To understand the processes that control the concentrations of geochemical species used for proxies of the past environment, both in the water column and in the substrates that reflect the water column.

GEOTRACES will be global in scope, consisting of ocean sections complemented by regional process studies. Sections and process studies will combine fieldwork, laboratory experiments and modelling. Beyond realizing the scientific objectives identified above, a natural outcome of this work will be to build a community of marine scientists who understand the processes regulating trace element cycles sufficiently well to exploit this knowledge reliably in future interdisciplinary studies.
Expand &quot;Projects&quot; below for information about and data resulting from individual US GEOTRACES research projects.</gco:CharacterString>
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                            <gco:CharacterString>&lt;p&gt;&lt;em&gt;Much of this text appeared in an article published in OCB News, October 2008, by the OCB Project Office.&lt;/em&gt;&lt;/p&gt;
&lt;p&gt;The first U.S. GEOTRACES Atlantic Section will be specifically centered around a sampling cruise to be carried out in the North Atlantic in 2010. Ed Boyle (MIT) and Bill Jenkins (WHOI) organized a three-day planning workshop that was held September 22-24, 2008 at the Woods Hole Oceanographic Institution. The main goal of the workshop, sponsored by the National Science Foundation and the U.S. GEOTRACES Scientific Steering Committee, was to design the implementation plan for the first U.S. GEOTRACES Atlantic Section. The primary cruise design motivation was to improve knowledge of the sources, sinks and internal cycling of Trace Elements and their Isotopes (TEIs) by studying their distributions along a section in the North Atlantic (Figure 1). The North Atlantic has the full suite of processes that affect TEIs, including strong meridional advection, boundary scavenging and source effects, aeolian deposition, and the salty Mediterranean Outflow. The North Atlantic is particularly important as it lies at the &quot;origin&quot; of the global Meridional Overturning Circulation.&lt;/p&gt;
&lt;p&gt;It is well understood that many trace metals play important roles in biogeochemical processes and the carbon cycle, yet very little is known about their large-scale distributions and the regional scale processes that affect them. Recent advances in sampling and analytical techniques, along with advances in our understanding of their roles in enzymatic and catalytic processes in the open ocean provide a natural opportunity to make substantial advances in our understanding of these important elements. Moreover, we are motivated by the prospect of global change and the need to understand the present and future workings of the ocean's biogeochemistry. The GEOTRACES strategy is to measure a broad suite of TEIs to constrain the critical biogeochemical processes that influence their distributions. In addition to these &quot;exotic&quot; substances, more traditional properties, including macronutrients (at micromolar and nanomolar levels), CTD, bio-optical parameters, and carbon system characteristics will be measured. The cruise starts at Line W, a repeat hydrographic section southeast of Cape Cod, extends to Bermuda and subsequently through the North Atlantic oligotrophic subtropical gyre, then transects into the African coast in the northern limb of the coastal upwelling region. From there, the cruise goes northward into the Mediterranean outflow. The station locations shown on the map are for the &quot;fulldepth TEI&quot; stations, and constitute approximately half of the stations to be ultimately occupied.&lt;/p&gt;
&lt;p&gt;&lt;em&gt;Figure 1. The proposed 2010 Atlantic GEOTRACES cruise track plotted on dissolved oxygen at 400 m depth. Data from the World Ocean Atlas (Levitus et al., 2005) were plotted using Ocean Data View (courtesy Reiner Schlitzer). [click on the image to view a larger version]&lt;/em&gt;&lt;br /&gt;
&lt;a href=&quot;http://bcodata.whoi.edu/US_GEOTRACES/AtlanticSection/GEOTRACES_Atl_stas.jpg&quot; target=&quot;_blank&quot;&gt;&lt;img alt=&quot;&quot; src=&quot;https://datadocs.bco-dmo.org/d2/US_GEOTRACES/AtlanticSection/GEOTRACES_Atl_stas.jpg&quot; style=&quot;width:350px&quot; /&gt;&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;Hydrography, CTD and nutrient measurements will be supported by the Ocean Data Facility (J. Swift) at Scripps Institution of Oceanography and funded through NSF Facilities. They will be providing an additional CTD rosette system along with nephelometer and LADCP. A trace metal clean Go-Flo Rosette and winch will be provided by the group at Old Dominion University (G. Cutter) along with a towed underway pumping system.&lt;/p&gt;
&lt;p&gt;The North Atlantic Transect cruise began in 2010 with KN199 leg 4 (station sampling) and leg 5 (underway sampling only) (Figure 2).&lt;/p&gt;
&lt;p&gt;&lt;a href=&quot;http://bcodata.whoi.edu//US_GEOTRACES/AtlanticSection/Cruise_Report_for_Knorr_199_Final_v3.pdf&quot; target=&quot;_blank&quot;&gt;KN199-04 Cruise Report (PDF)&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&lt;em&gt;Figure 2. The red line shows the cruise track for the first leg of the US Geotraces North Atlantic Transect on the R/V Knorr in October 2010.  The rest of the stations (beginning with 13) will be completed in October-December 2011 on the R/V Knorr (courtesy of Bill Jenkins, Chief Scientist, GNAT first leg). [click on the image to view a larger version]&lt;/em&gt;&lt;br /&gt;
&lt;a href=&quot;http://bcodata.whoi.edu/US_GEOTRACES/AtlanticSection/GNAT_stationPlan.jpg&quot; target=&quot;_blank&quot;&gt;&lt;img alt=&quot;Atlantic Transect Station location map&quot; src=&quot;https://datadocs.bco-dmo.org/d2/US_GEOTRACES/AtlanticSection/GNAT_stationPlan_sm.jpg&quot; style=&quot;width:350px&quot; /&gt;&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;The section completion effort resumed again in November 2011 with KN204-01A,B (Figure 3).&lt;/p&gt;
&lt;p&gt;&lt;a href=&quot;http://bcodata.whoi.edu//US_GEOTRACES/AtlanticSection/Submitted_Preliminary_Cruise_Report_for_Knorr_204-01.pdf&quot; target=&quot;_blank&quot;&gt;KN204-01A,B Cruise Report (PDF)&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&lt;em&gt;Figure 3. Station locations occupied on the US Geotraces North Atlantic Transect on the R/V Knorr in November 2011.  [click on the image to view a larger version]&lt;/em&gt;&lt;br /&gt;
&lt;a href=&quot;http://bcodata.whoi.edu/US_GEOTRACES/AtlanticSection/KN204-01_Stations.png&quot; target=&quot;_blank&quot;&gt;&lt;img alt=&quot;Atlantic Transect/Part 2 Station location map&quot; src=&quot;https://datadocs.bco-dmo.org/d2/US_GEOTRACES/AtlanticSection/KN204-01_Stations.png&quot; style=&quot;width:350px&quot; /&gt;&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;Data from the North Atlantic Transect cruises are available under the Datasets heading below, and consensus values for the SAFe and North Atlantic GEOTRACES Reference Seawater Samples are available from the GEOTRACES Program Office: &lt;a href=&quot;http://www.geotraces.org/science/intercalibration/322-standards-and-reference-materials?acm=455_215&quot; target=&quot;_blank&quot;&gt;Standards and Reference Materials&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;ADCP data&lt;/strong&gt; are available from the Currents ADCP group at the University of Hawaii at the links below:&lt;br /&gt;
&lt;a href=&quot;http://currents.soest.hawaii.edu/uhdas_adcp/year2010.html#kn199_4&quot; target=&quot;_blank&quot;&gt;KN199-04&lt;/a&gt;   (leg 1 of 2010 cruise; Lisbon to Cape Verde)&lt;br /&gt;
&lt;a href=&quot;http://currents.soest.hawaii.edu/uhdas_adcp/year2010.html#kn199_5&quot; target=&quot;_blank&quot;&gt;KN199-05&lt;/a&gt;   (leg 2 of 2010 cruise; Cape Verde to Charleston, NC)&lt;br /&gt;
&lt;a href=&quot;http://currents.soest.hawaii.edu/uhdas_adcp/year2011.html#kn204_01&quot; target=&quot;_blank&quot;&gt;KN204-01A&lt;/a&gt; (part 1 of 2011 cruise; Woods Hole, MA to Bermuda)&lt;br /&gt;
&lt;a href=&quot;http://currents.soest.hawaii.edu/uhdas_adcp/year2011.html#kn204_02&quot; target=&quot;_blank&quot;&gt;KN204-01B&lt;/a&gt; (part 2 of 2011 cruise; Bermuda to Cape Verde)&lt;/p&gt;</gco:CharacterString>
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            http://lod.bco-dmo.org/id/dataset-parameter/31588.rdf
	Name: cruise_id
	Units: text
	Description: &lt;p&gt;Official cruise identifier e.g. KN199-04 = R/V Knorr cruise number 199-04.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31589.rdf
	Name: cruise_part
	Units: text
	Description: &lt;p&gt;Part of cruise. For KN204-01:&lt;br /&gt;&lt;br /&gt;
A = 11/6/2011 to 11/18/2011 (Woods Hole to Bermuda)&lt;br /&gt;&lt;br /&gt;
B = 11/19/2011 to 12/11/2011 (Bermuda to Praia, Cabo Verde)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31590.rdf
	Name: station_GEOTRC
	Units: unitless
	Description: &lt;p&gt;GEOTRACES station number; ranges from 1 through 12 for KN199-04 and 1 through 24 for KN204-01. Stations 7 and 9 were skipped on KN204-01. PI-supplied values were identical to those in the&lt;br /&gt;
intermediate US GEOTRACES master file. Originally submitted as 'Station', this parameter name has been changed to conform to BCO-DMO's GEOTRACES naming conventions.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31591.rdf
	Name: lat
	Units: decimal degrees
	Description: &lt;p&gt;Latitude. Positive = North.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31592.rdf
	Name: lon
	Units: decimal degrees
	Description: &lt;p&gt;Longitude. Negative = West.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31593.rdf
	Name: event
	Units: unitless
	Description: &lt;p&gt;GEOTRACES event number; provided in original data submission.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31594.rdf
	Name: cast_GEOTRC
	Units: unitless
	Description: &lt;p&gt;Cast identifier, numbered consecutively within a station. PI-supplied values were identical to those in the intermediate US GEOTRACES master file. Originally submitted as 'Cast', &lt;br /&gt;this parameter name has been changed to conform to BCO-DMO's GEOTRACES naming conventions.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31595.rdf
	Name: month_gmt
	Units: unitless
	Description: &lt;p&gt;2-digit month of year (GMT). in the format mm (01 to 12)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31596.rdf
	Name: day_gmt
	Units: unitless
	Description: &lt;p&gt;2-digit day of month (GMT). in the format dd (01 to 31)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31597.rdf
	Name: year
	Units: unitless
	Description: &lt;p&gt;4-digit year. in the format YYYY&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31598.rdf
	Name: time_gmt
	Units: unitless
	Description: &lt;p&gt;Time (GMT); 24-hour clock. in the format HHMM&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31599.rdf
	Name: bottle
	Units: unitless
	Description: &lt;p&gt;Bottle number; provided in original data submission.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31600.rdf
	Name: sample_GEOTRC
	Units: unitless
	Description: &lt;p&gt;Unique identifying number for US GEOTRACES samples; ranges from 5033 to 6078 for KN199-04 and from 6112 to 8148 for KN204-01. PI-supplied values were identical to those in the &lt;br /&gt;intermediate US GEOTRACES master file. Originally submitted as 'Geotraces #', this parameter name has been changed to conform to BCO-DMO's GEOTRACES naming conventions.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31601.rdf
	Name: depth_n
	Units: meters
	Description: &lt;p&gt;Nominal sample depth.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/31602.rdf
	Name: depth
	Units: meters
	Description: &lt;p&gt;Actual sample depth; provided in original data submission.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/32087.rdf
	Name: U238
	Units: dpm/Liter
	Description: &lt;p&gt;Total Uranium-238 concentration. Includes dissolved + particulate (though particulate fraction is very small).&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/32088.rdf
	Name: U238_unc
	Units: dpm/Liter
	Description: &lt;p&gt;U238 uncertainty. Derived from the uncertainty in the relationship in Owens et al. (2011).&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/32089.rdf
	Name: Th234_tot
	Units: dpm/Liter
	Description: &lt;p&gt;Thorium-234 concentration.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/32090.rdf
	Name: Th_234_tot_unc
	Units: dpm/Liter
	Description: &lt;p&gt;Th234 uncertainty. Derived from counting statistics.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/32091.rdf
	Name: q_flag
	Units: unitless
	Description: &lt;p&gt;Quality flag:&lt;br /&gt;
1 = Good&lt;br /&gt;
2 = Questionable&lt;br /&gt;
3 = Bad&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33195.rdf
	Name: depth_GEOTRC_CTD
	Units: meters
	Description: &lt;p&gt;Observation/sample depth in meters, calculated from CTD pressure. Values were added from the intermediate US GEOTRACES master file (see Processing Description).&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33196.rdf
	Name: event_GEOTRC
	Units: unitless
	Description: &lt;p&gt;Unique identifying number for US GEOTRACES sampling events; ranges from 2001 to 2225 for KN199-04 events and from 3001 to 3282 for KN204-01 events. &lt;br /&gt;Values were added from the intermediate US GEOTRACES master file (see Processing Description).&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33197.rdf
	Name: sample_bottle_GEOTRC
	Units: unitless
	Description: &lt;p&gt;Unique identification numbers given to samples taken from bottles; ranges from 1 to 24; often used synonymously with bottle number.&lt;br /&gt; Values were added from the intermediate US GEOTRACES master file (see Processing Description). &lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33198.rdf
	Name: bottle_GEOTRC
	Units: unitless
	Description: &lt;p&gt;Alphanumeric characters identifying bottle type (e.g., NIS representing Niskin and GF representing GOFLO) and position on a CTD rosette.&lt;br /&gt; Values were added from the intermediate US GEOTRACES master file (see Processing Description).&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33199.rdf
	Name: Cast_ISO_DateTime_UTC
	Units: yyyy-MM-dd&amp;#039;T&amp;#039;HH:mm:ss.SS&amp;#039;Z&amp;#039;
	Description: &lt;p&gt;Cast date/time (UTC) formatted to ISO8601 standard. T indicates start of time string; Z indicates UTC. Calculated from original date and time fields.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33200.rdf
	Name: BTL_ISO_DateTime_UTC
	Units: unitless
	Description: &lt;p&gt;Date and time (UTC) variable recorded at the bottle sampling time in ISO compliant format. Values were added from the intermediate US GEOTRACES master file (see Processing Description).&lt;br /&gt;
This standard is based on ISO 8601:2004(E) and takes on the following form: 2009-08-30T14:05:00[.xx]Z (UTC time)&lt;/p&gt; 
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                <gco:CharacterString>&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Uranium-238&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Value and uncertainty from equation derived in Owens et al. (2011)&amp;lt;br /&amp;gt;
&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp; &amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp; U-238 (dpm/L) = (Salinity * 0.0786) - 0.315&amp;lt;br /&amp;gt;
Salinity was measured onboard the ship by the Scripps Ocean Data Facility.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Thorium-234&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Determined by the widely-adopted 4 L method. Shallow (&amp;amp;lt; 1000 m) samples were collected from the SIO ODF Rosette and deep samples (&amp;amp;gt;1000 m) were collected from Niskin bottles hung above in situ pumps. Data are decay corrected to the mid-point time between when bottles 1 and 12 were fired for shallow casts and when the messenger was dropped for deep cast. All surface samples were collected using a deck-mounted pump (denoted as bottle 13). All data have been recovery-corrected using the Th-230/Th-229 recovery method (see references below) to account for any loss of sample material during processing. All samples were analyzed using RISO Laboratory Anti-coincidence Beta Counters, using a helium/1% butane mixture. Overall method efficiency was determined by minimizing the percent difference between mean U-238 and Th-234 values for samples from &amp;amp;gt;1000 m to &amp;amp;gt; 1000 m from the bottom (44.5 % for KN 199-4 and 46.4 % for KN 204-01a and KN 204-01b).&amp;lt;/p&amp;gt;</gco:CharacterString>
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              <gmd:description>
                <gco:CharacterString>&amp;lt;p&amp;gt;Data were flagged with quality indicators: 1 = Good; 2 = Questionable; 3 = Bad.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;BCO-DMO made the following modifications:&amp;lt;br /&amp;gt;
- Parameter names have been modified to conform with BCO-DMO naming conventions.&amp;lt;br /&amp;gt;
- cruise_part was separated from the official cruise ID for cruise KN204-01.&amp;lt;br /&amp;gt;
- Added Cast_ISO_DateTime_UTC from the original cast dates and times.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Additional GEOTRACES Processing:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
After the data were submitted to the International Data Management Office, BODC, the office noticed that important identifying information was missing in many datasets. With the agreement of BODC and the US GEOTRACES lead PIs, BCO-DMO added standard US GEOTRACES information, such as the US GEOTRACES event number, to each submitted dataset lacking this information. To accomplish this, BCO-DMO compiled a 'master' dataset composed of the following parameters: station_GEOTRC, cast_GEOTRC (bottle and pump data only), event_GEOTRC, sample_GEOTRC, sample_bottle_GEOTRC (bottle data only), bottle_GEOTRC (bottle data only), depth_GEOTRC_CTD (bottle data only), depth_GEOTRC_CTD_rounded (bottle data only), BTL_ISO_DateTime_UTC (bottle data only), and GeoFish_id (GeoFish data only). This added information will facilitate subsequent analysis and inter comparison of the datasets.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
Bottle parameters in the master file were taken from the GT-C_Bottle_GT10, GT-C_Bottle_GT11, ODF_Bottle_GT10, and ODF_Bottle_GT11 datasets. Non-bottle parameters, including those from GeoFish tows, Aerosol sampling, and McLane Pumps, were taken from the Event_Log_GT10 and Event_Log_GT11 datasets. McLane pump cast numbers missing in event logs were taken from the Particulate Th-234 dataset submitted by Ken Buesseler.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
A standardized BCO-DMO method (called &amp;quot;join&amp;quot;) was then used to merge the missing parameters to each US GEOTRACES dataset, most often by matching on sample_GEOTRC or on some unique combination of other parameters.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
If the master parameters were included in the original data file and the values did not differ from the master file, the original data columns were retained and the names of the parameters were changed from the PI-submitted names to the standardized master names. If there were differences between the PI-supplied parameter values and those in the master file, both columns were retained. If the original data submission included all of the master parameters, no additional columns were added, but parameter names were modified to match the naming conventions of the master file.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
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