Diffusion Aspects of Designing Porous Growth Media for Earth and Space
Growing plants in extraterrestrial environments, for example on a space station or in a future lunar or Martian outpost, is a challenge that has attracted increasing interest over the last few decades. Most of the essential plant needs for optimal growth (air, water, and nutrient supply, and mechani...
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creator | Deepagoda, T.K.K. Chamindu Moldrup, Per Jensen, Maria P Jones, Scott B Jonge, Lis Wollesen de Schjonning, Per Scow, Kate Hopmans, Jan W Rolston, Dennis E Kawamoto, Ken Komatsu, Toshiko |
description | Growing plants in extraterrestrial environments, for example on a space station or in a future lunar or Martian outpost, is a challenge that has attracted increasing interest over the last few decades. Most of the essential plant needs for optimal growth (air, water, and nutrient supply, and mechanical support) are closely linked with the basic physical properties of the growth media. Diffusion is the main process whereby oxygen and nutrients are supplied to plant roots, and gas and solute diffusivity are the key parameters controlling the diffusive movement of oxygen and nutrients in the root zone. As one among several essential aspects of optimal porous media design for plant growth, this study presents a diffusion-based characterization of four commercial, aggregated growth media. To account for the observed large percolation threshold for gas diffusivity in the selected media, an inactive pore and density corrected (IPDC) model was developed and excellently described measured gas diffusivity in both inter- and intraaggregate pore regions. A strong relation (r2 = 0.98) between percolation threshold for gas diffusivity and mean particle (aggregate) diameter was found and suggested to be used in future design models. Also, critical windows of diffusivity (CWD) was defined identifying the air content range where gas diffusivity (hence, oxygen supply) and solute diffusivity or the analogous electrical conductivity (hence, nutrient supply) are above pre-defined, critical minimum values. Assuming different critical values for gas diffusivity under terrestrial and Martian conditions, the four growth media were compared and it was found that one medium did not fulfill the pre-set criteria. Overall, the analyses suggested that particle (aggregate) sizes below 0.25 and above 5 mm should likely be avoided when designing safe plant growth media for space. The CWD concept was also applied to a natural volcanic ash soil (Nishi-Tokyo, Japan), and the natural soil was found competitive or better than the tested commercial growth media. This could bear large perspectives for Martian outpost missions, since NASA has found that Martian dust/soil mostly resembles volcanic ash soil among terrestrial materials. |
doi_str_mv | 10.2136/sssaj2011.0438 |
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Chamindu ; Moldrup, Per ; Jensen, Maria P ; Jones, Scott B ; Jonge, Lis Wollesen de ; Schjonning, Per ; Scow, Kate ; Hopmans, Jan W ; Rolston, Dennis E ; Kawamoto, Ken ; Komatsu, Toshiko</creator><creatorcontrib>Deepagoda, T.K.K. Chamindu ; Moldrup, Per ; Jensen, Maria P ; Jones, Scott B ; Jonge, Lis Wollesen de ; Schjonning, Per ; Scow, Kate ; Hopmans, Jan W ; Rolston, Dennis E ; Kawamoto, Ken ; Komatsu, Toshiko</creatorcontrib><description>Growing plants in extraterrestrial environments, for example on a space station or in a future lunar or Martian outpost, is a challenge that has attracted increasing interest over the last few decades. Most of the essential plant needs for optimal growth (air, water, and nutrient supply, and mechanical support) are closely linked with the basic physical properties of the growth media. Diffusion is the main process whereby oxygen and nutrients are supplied to plant roots, and gas and solute diffusivity are the key parameters controlling the diffusive movement of oxygen and nutrients in the root zone. As one among several essential aspects of optimal porous media design for plant growth, this study presents a diffusion-based characterization of four commercial, aggregated growth media. To account for the observed large percolation threshold for gas diffusivity in the selected media, an inactive pore and density corrected (IPDC) model was developed and excellently described measured gas diffusivity in both inter- and intraaggregate pore regions. A strong relation (r2 = 0.98) between percolation threshold for gas diffusivity and mean particle (aggregate) diameter was found and suggested to be used in future design models. Also, critical windows of diffusivity (CWD) was defined identifying the air content range where gas diffusivity (hence, oxygen supply) and solute diffusivity or the analogous electrical conductivity (hence, nutrient supply) are above pre-defined, critical minimum values. Assuming different critical values for gas diffusivity under terrestrial and Martian conditions, the four growth media were compared and it was found that one medium did not fulfill the pre-set criteria. Overall, the analyses suggested that particle (aggregate) sizes below 0.25 and above 5 mm should likely be avoided when designing safe plant growth media for space. The CWD concept was also applied to a natural volcanic ash soil (Nishi-Tokyo, Japan), and the natural soil was found competitive or better than the tested commercial growth media. 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Chamindu</creatorcontrib><creatorcontrib>Moldrup, Per</creatorcontrib><creatorcontrib>Jensen, Maria P</creatorcontrib><creatorcontrib>Jones, Scott B</creatorcontrib><creatorcontrib>Jonge, Lis Wollesen de</creatorcontrib><creatorcontrib>Schjonning, Per</creatorcontrib><creatorcontrib>Scow, Kate</creatorcontrib><creatorcontrib>Hopmans, Jan W</creatorcontrib><creatorcontrib>Rolston, Dennis E</creatorcontrib><creatorcontrib>Kawamoto, Ken</creatorcontrib><creatorcontrib>Komatsu, Toshiko</creatorcontrib><title>Diffusion Aspects of Designing Porous Growth Media for Earth and Space</title><title>Soil Science Society of America journal</title><description>Growing plants in extraterrestrial environments, for example on a space station or in a future lunar or Martian outpost, is a challenge that has attracted increasing interest over the last few decades. Most of the essential plant needs for optimal growth (air, water, and nutrient supply, and mechanical support) are closely linked with the basic physical properties of the growth media. Diffusion is the main process whereby oxygen and nutrients are supplied to plant roots, and gas and solute diffusivity are the key parameters controlling the diffusive movement of oxygen and nutrients in the root zone. As one among several essential aspects of optimal porous media design for plant growth, this study presents a diffusion-based characterization of four commercial, aggregated growth media. To account for the observed large percolation threshold for gas diffusivity in the selected media, an inactive pore and density corrected (IPDC) model was developed and excellently described measured gas diffusivity in both inter- and intraaggregate pore regions. A strong relation (r2 = 0.98) between percolation threshold for gas diffusivity and mean particle (aggregate) diameter was found and suggested to be used in future design models. Also, critical windows of diffusivity (CWD) was defined identifying the air content range where gas diffusivity (hence, oxygen supply) and solute diffusivity or the analogous electrical conductivity (hence, nutrient supply) are above pre-defined, critical minimum values. Assuming different critical values for gas diffusivity under terrestrial and Martian conditions, the four growth media were compared and it was found that one medium did not fulfill the pre-set criteria. Overall, the analyses suggested that particle (aggregate) sizes below 0.25 and above 5 mm should likely be avoided when designing safe plant growth media for space. The CWD concept was also applied to a natural volcanic ash soil (Nishi-Tokyo, Japan), and the natural soil was found competitive or better than the tested commercial growth media. This could bear large perspectives for Martian outpost missions, since NASA has found that Martian dust/soil mostly resembles volcanic ash soil among terrestrial materials.</description><subject>Agronomy. Soil science and plant productions</subject><subject>air</subject><subject>Atoms & subatomic particles</subject><subject>Biological and medical sciences</subject><subject>culture media</subject><subject>diffusivity</subject><subject>Earth</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>electrical conductivity</subject><subject>Exact sciences and technology</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Gases</subject><subject>Gravity</subject><subject>growing media</subject><subject>Growth media</subject><subject>Life support systems</subject><subject>Mars</subject><subject>Nutrients</subject><subject>Oxygen</subject><subject>Percolation</subject><subject>Physical properties</subject><subject>Plant growth</subject><subject>Pore size</subject><subject>Porous media</subject><subject>rhizosphere</subject><subject>Root zone</subject><subject>roots</subject><subject>Soil science</subject><subject>Soils</subject><subject>solutes</subject><subject>Studies</subject><subject>Surficial geology</subject><subject>volcanic ash soils</subject><subject>Volcanic soils</subject><issn>0361-5995</issn><issn>1435-0661</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqFkc9LwzAcxYMoOKdXrwbEY2e-SZqlBw_D_VCZKNSdS5oms2M2NVkZ--_N2NjVS758k897D14QugUyoMDEYwhBrSgBGBDO5BnqAWdpQoSAc9QjTECSZll6ia5CWBECaUZID03HtbVdqF2DR6E1ehOws3hsQr1s6maJP513XcAz77abb_xuqlph6zyeKB931VQ4b5U21-jCqnUwN8fZR4vp5Ov5JZl_zF6fR_NEc0hlQk1MrSrQpNI2K6m1qWWcC8UYUGVYCUpboVXJhhQMiApkKSRURpNUalmyPro_-Lbe_XYmbIqV63wTIwsgUjAuKZeRGhwo7V0I3tii9fWP8rsIFfuuilNXxb6rKHg42qqg1dp61eg6nFRUsCwbUhq5pwO3rddm949rkY_eaJ7vz3h1zLk76K1yhVr6mLHI4yuP_8FlOpTsDxEphSY</recordid><startdate>201209</startdate><enddate>201209</enddate><creator>Deepagoda, T.K.K. 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Chamindu ; Moldrup, Per ; Jensen, Maria P ; Jones, Scott B ; Jonge, Lis Wollesen de ; Schjonning, Per ; Scow, Kate ; Hopmans, Jan W ; Rolston, Dennis E ; Kawamoto, Ken ; Komatsu, Toshiko</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4158-2e590dd1c0dcf9b2ff5f3446a3312ae3b1acf6cab3721e16d18b681dec058c8b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Agronomy. Soil science and plant productions</topic><topic>air</topic><topic>Atoms & subatomic particles</topic><topic>Biological and medical sciences</topic><topic>culture media</topic><topic>diffusivity</topic><topic>Earth</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>electrical conductivity</topic><topic>Exact sciences and technology</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Gases</topic><topic>Gravity</topic><topic>growing media</topic><topic>Growth media</topic><topic>Life support systems</topic><topic>Mars</topic><topic>Nutrients</topic><topic>Oxygen</topic><topic>Percolation</topic><topic>Physical properties</topic><topic>Plant growth</topic><topic>Pore size</topic><topic>Porous media</topic><topic>rhizosphere</topic><topic>Root zone</topic><topic>roots</topic><topic>Soil science</topic><topic>Soils</topic><topic>solutes</topic><topic>Studies</topic><topic>Surficial geology</topic><topic>volcanic ash soils</topic><topic>Volcanic soils</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Deepagoda, T.K.K. 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Chamindu</au><au>Moldrup, Per</au><au>Jensen, Maria P</au><au>Jones, Scott B</au><au>Jonge, Lis Wollesen de</au><au>Schjonning, Per</au><au>Scow, Kate</au><au>Hopmans, Jan W</au><au>Rolston, Dennis E</au><au>Kawamoto, Ken</au><au>Komatsu, Toshiko</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Diffusion Aspects of Designing Porous Growth Media for Earth and Space</atitle><jtitle>Soil Science Society of America journal</jtitle><date>2012-09</date><risdate>2012</risdate><volume>76</volume><issue>5</issue><spage>1564</spage><epage>1578</epage><pages>1564-1578</pages><issn>0361-5995</issn><eissn>1435-0661</eissn><coden>SSSJD4</coden><abstract>Growing plants in extraterrestrial environments, for example on a space station or in a future lunar or Martian outpost, is a challenge that has attracted increasing interest over the last few decades. Most of the essential plant needs for optimal growth (air, water, and nutrient supply, and mechanical support) are closely linked with the basic physical properties of the growth media. Diffusion is the main process whereby oxygen and nutrients are supplied to plant roots, and gas and solute diffusivity are the key parameters controlling the diffusive movement of oxygen and nutrients in the root zone. As one among several essential aspects of optimal porous media design for plant growth, this study presents a diffusion-based characterization of four commercial, aggregated growth media. To account for the observed large percolation threshold for gas diffusivity in the selected media, an inactive pore and density corrected (IPDC) model was developed and excellently described measured gas diffusivity in both inter- and intraaggregate pore regions. A strong relation (r2 = 0.98) between percolation threshold for gas diffusivity and mean particle (aggregate) diameter was found and suggested to be used in future design models. Also, critical windows of diffusivity (CWD) was defined identifying the air content range where gas diffusivity (hence, oxygen supply) and solute diffusivity or the analogous electrical conductivity (hence, nutrient supply) are above pre-defined, critical minimum values. Assuming different critical values for gas diffusivity under terrestrial and Martian conditions, the four growth media were compared and it was found that one medium did not fulfill the pre-set criteria. Overall, the analyses suggested that particle (aggregate) sizes below 0.25 and above 5 mm should likely be avoided when designing safe plant growth media for space. The CWD concept was also applied to a natural volcanic ash soil (Nishi-Tokyo, Japan), and the natural soil was found competitive or better than the tested commercial growth media. This could bear large perspectives for Martian outpost missions, since NASA has found that Martian dust/soil mostly resembles volcanic ash soil among terrestrial materials.</abstract><cop>Madison, WI</cop><pub>Soil Science Society of America</pub><doi>10.2136/sssaj2011.0438</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Agronomy. Soil science and plant productions air Atoms & subatomic particles Biological and medical sciences culture media diffusivity Earth Earth sciences Earth, ocean, space electrical conductivity Exact sciences and technology Fundamental and applied biological sciences. Psychology Gases Gravity growing media Growth media Life support systems Mars Nutrients Oxygen Percolation Physical properties Plant growth Pore size Porous media rhizosphere Root zone roots Soil science Soils solutes Studies Surficial geology volcanic ash soils Volcanic soils |
title | Diffusion Aspects of Designing Porous Growth Media for Earth and Space |
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