The Design and Development of a Closed Chamber for the in-situ Quantification of Dryland Soil Carbon Dioxide Fluxes
This paper describes the design features and capabilities of a portable automated in‐situ closed chamber (ISCC) for the quantification of CO2 fluxes in dryland soils where both photosynthetic and respiratory components may be associated with a cyanobacterial crust. The processes of CO2 flux in dryla...
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description | This paper describes the design features and capabilities of a portable automated in‐situ closed chamber (ISCC) for the quantification of CO2 fluxes in dryland soils where both photosynthetic and respiratory components may be associated with a cyanobacterial crust. The processes of CO2 flux in dryland soils are briefly described in order to clarify the conditions that make quantification of these fluxes problematic. The instrumentation currently available for in‐situ soil CO2 flux measurements is then reviewed demonstrating their inadequacies for the dryland environment. The ISCC described here is a member of the closed or enrichment class of soil respiration chambers. The ISCC, however, features an optical window possessing high (>90%) transmission in the photosynthetic active region (PAR) of the solar irradiance spectrum, permitting observations of photosynthesis. The ISCC possesses automatic venting and purging so that gaseous concentrations inside the chamber do not change from ambient sufficiently to significantly affect diffusion. The ISCC features both active and passive cooling employing internal solid‐state Peltier coolers and external aluminised Mylar respectively. This avoids severe disturbance of the microclimate within the chamber due to admission of high fluxes of PAR and permits in‐situ operation under a wide range of ambient field temperatures (~ −5 to 40°C). Sensors internal to the chamber monitor temperature, relative humidity, irradiance and pressure. In this implementation the ISCC is coupled to a portable gas chromatograph (Agilent GC‐3000) to sample the chamber atmosphere. Indicative data for Kalahari Sand soils of Botswana are presented as an illustration of the general performance characteristics. |
doi_str_mv | 10.1111/j.1745-5871.2008.00551.x |
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The processes of CO2 flux in dryland soils are briefly described in order to clarify the conditions that make quantification of these fluxes problematic. The instrumentation currently available for in‐situ soil CO2 flux measurements is then reviewed demonstrating their inadequacies for the dryland environment. The ISCC described here is a member of the closed or enrichment class of soil respiration chambers. The ISCC, however, features an optical window possessing high (>90%) transmission in the photosynthetic active region (PAR) of the solar irradiance spectrum, permitting observations of photosynthesis. The ISCC possesses automatic venting and purging so that gaseous concentrations inside the chamber do not change from ambient sufficiently to significantly affect diffusion. The ISCC features both active and passive cooling employing internal solid‐state Peltier coolers and external aluminised Mylar respectively. This avoids severe disturbance of the microclimate within the chamber due to admission of high fluxes of PAR and permits in‐situ operation under a wide range of ambient field temperatures (~ −5 to 40°C). Sensors internal to the chamber monitor temperature, relative humidity, irradiance and pressure. In this implementation the ISCC is coupled to a portable gas chromatograph (Agilent GC‐3000) to sample the chamber atmosphere. Indicative data for Kalahari Sand soils of Botswana are presented as an illustration of the general performance characteristics.</description><identifier>ISSN: 1745-5863</identifier><identifier>EISSN: 1745-5871</identifier><identifier>DOI: 10.1111/j.1745-5871.2008.00551.x</identifier><language>eng</language><publisher>Melbourne, Australia: Blackwell Publishing Asia</publisher><subject>Africa ; Arid zones ; Botswana ; Cyanobacterial soil crusts ; Desert ; drylands ; Ecology ; Environmental degradation ; Geography ; Kalahari ; Land ; Photosynthetically active radiation ; soil CO2 flux ; Soil erosion ; Soil respiration chambers ; Soils</subject><ispartof>Geographical research, 2009-03, Vol.47 (1), p.71-82</ispartof><rights>2008 The Authors. 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The processes of CO2 flux in dryland soils are briefly described in order to clarify the conditions that make quantification of these fluxes problematic. The instrumentation currently available for in‐situ soil CO2 flux measurements is then reviewed demonstrating their inadequacies for the dryland environment. The ISCC described here is a member of the closed or enrichment class of soil respiration chambers. The ISCC, however, features an optical window possessing high (>90%) transmission in the photosynthetic active region (PAR) of the solar irradiance spectrum, permitting observations of photosynthesis. The ISCC possesses automatic venting and purging so that gaseous concentrations inside the chamber do not change from ambient sufficiently to significantly affect diffusion. The ISCC features both active and passive cooling employing internal solid‐state Peltier coolers and external aluminised Mylar respectively. This avoids severe disturbance of the microclimate within the chamber due to admission of high fluxes of PAR and permits in‐situ operation under a wide range of ambient field temperatures (~ −5 to 40°C). Sensors internal to the chamber monitor temperature, relative humidity, irradiance and pressure. In this implementation the ISCC is coupled to a portable gas chromatograph (Agilent GC‐3000) to sample the chamber atmosphere. Indicative data for Kalahari Sand soils of Botswana are presented as an illustration of the general performance characteristics.</description><subject>Africa</subject><subject>Arid zones</subject><subject>Botswana</subject><subject>Cyanobacterial soil crusts</subject><subject>Desert</subject><subject>drylands</subject><subject>Ecology</subject><subject>Environmental degradation</subject><subject>Geography</subject><subject>Kalahari</subject><subject>Land</subject><subject>Photosynthetically active radiation</subject><subject>soil CO2 flux</subject><subject>Soil erosion</subject><subject>Soil respiration chambers</subject><subject>Soils</subject><issn>1745-5863</issn><issn>1745-5871</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><recordid>eNqNUU2P1CAYbowmrqv_gZO3VihQ2oMHt7Mzmqxu1NU9vqGF7jC2ZRaodv691Jq5Khee8Hzk5X2SBBGckXjeHDIiGE95KUiWY1xmGHNOsvlJcnEmnp5xQZ8nL7w_YEwLXrKLxN_tNdpobx5GJEcV4U_d2-Ogx4BshySqe-u1QvVeDo12qLMOhWgxY-pNmNDnSY7BdKaVwdhxsWzcqV-SvlrTo1q6Jj5vjJ2N0mjbT7P2L5Nnney9fvX3vky-ba_v6vfpze3uQ_3uJpWsqkiaC8Vlq3ijSyIoywkmggvSlJUSWCjcxe9GtmyKluS0a1nbMKWwVqKSLFL0Mnm95h6dfZy0DzAY3-o-jqft5IEKQquciX8Kc5KziuYsCstV2DrrvdMdHJ0ZpDsBwbDUAQdYNg3L1mGpA_7UAXO0vl2tv0yvT__tg9317ZeIon-7-t1gAsij7ALsQzh6UDJIMGNsZmGsewBlzRJMKSnA6D6Kl8wKU1EUMShdg4wPej4PIt0PKAQVHO4_7YBfVR_z4vs9XNHfwQu4aQ</recordid><startdate>200903</startdate><enddate>200903</enddate><creator>HOON, STEPHEN R.</creator><creator>THOMAS, ANDREW D.</creator><creator>LINTON, PATRICIA E</creator><general>Blackwell Publishing Asia</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>M7N</scope><scope>8BJ</scope><scope>FQK</scope><scope>JBE</scope></search><sort><creationdate>200903</creationdate><title>The Design and Development of a Closed Chamber for the in-situ Quantification of Dryland Soil Carbon Dioxide Fluxes</title><author>HOON, STEPHEN R. ; THOMAS, ANDREW D. ; LINTON, PATRICIA E</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4991-27d5acd5be8173421017571b89d707d0f200d5b8b6c123fc4cb4dd0ed79a400d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Africa</topic><topic>Arid zones</topic><topic>Botswana</topic><topic>Cyanobacterial soil crusts</topic><topic>Desert</topic><topic>drylands</topic><topic>Ecology</topic><topic>Environmental degradation</topic><topic>Geography</topic><topic>Kalahari</topic><topic>Land</topic><topic>Photosynthetically active radiation</topic><topic>soil CO2 flux</topic><topic>Soil erosion</topic><topic>Soil respiration chambers</topic><topic>Soils</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>HOON, STEPHEN R.</creatorcontrib><creatorcontrib>THOMAS, ANDREW D.</creatorcontrib><creatorcontrib>LINTON, PATRICIA E</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>International Bibliography of the Social Sciences (IBSS)</collection><collection>International Bibliography of the Social Sciences</collection><collection>International Bibliography of the Social Sciences</collection><jtitle>Geographical research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>HOON, STEPHEN R.</au><au>THOMAS, ANDREW D.</au><au>LINTON, PATRICIA E</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Design and Development of a Closed Chamber for the in-situ Quantification of Dryland Soil Carbon Dioxide Fluxes</atitle><jtitle>Geographical research</jtitle><date>2009-03</date><risdate>2009</risdate><volume>47</volume><issue>1</issue><spage>71</spage><epage>82</epage><pages>71-82</pages><issn>1745-5863</issn><eissn>1745-5871</eissn><abstract>This paper describes the design features and capabilities of a portable automated in‐situ closed chamber (ISCC) for the quantification of CO2 fluxes in dryland soils where both photosynthetic and respiratory components may be associated with a cyanobacterial crust. The processes of CO2 flux in dryland soils are briefly described in order to clarify the conditions that make quantification of these fluxes problematic. The instrumentation currently available for in‐situ soil CO2 flux measurements is then reviewed demonstrating their inadequacies for the dryland environment. The ISCC described here is a member of the closed or enrichment class of soil respiration chambers. The ISCC, however, features an optical window possessing high (>90%) transmission in the photosynthetic active region (PAR) of the solar irradiance spectrum, permitting observations of photosynthesis. The ISCC possesses automatic venting and purging so that gaseous concentrations inside the chamber do not change from ambient sufficiently to significantly affect diffusion. The ISCC features both active and passive cooling employing internal solid‐state Peltier coolers and external aluminised Mylar respectively. This avoids severe disturbance of the microclimate within the chamber due to admission of high fluxes of PAR and permits in‐situ operation under a wide range of ambient field temperatures (~ −5 to 40°C). Sensors internal to the chamber monitor temperature, relative humidity, irradiance and pressure. In this implementation the ISCC is coupled to a portable gas chromatograph (Agilent GC‐3000) to sample the chamber atmosphere. Indicative data for Kalahari Sand soils of Botswana are presented as an illustration of the general performance characteristics.</abstract><cop>Melbourne, Australia</cop><pub>Blackwell Publishing Asia</pub><doi>10.1111/j.1745-5871.2008.00551.x</doi><tpages>12</tpages></addata></record> |
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subjects | Africa Arid zones Botswana Cyanobacterial soil crusts Desert drylands Ecology Environmental degradation Geography Kalahari Land Photosynthetically active radiation soil CO2 flux Soil erosion Soil respiration chambers Soils |
title | The Design and Development of a Closed Chamber for the in-situ Quantification of Dryland Soil Carbon Dioxide Fluxes |
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