The effect of long-term atmospheric CO2 enrichment on the intrinsic water-use efficiency of sour orange trees
Every two months of 1992, as well as on three occasions in 1994-1995, we obtained leaf samples together with samples of surrounding air from eight well-watered and fertilized sour orange (Citrus aurantium L.) trees that were growing out-of-doors at Phoenix, Arizona, USA. These trees had been planted...
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Veröffentlicht in: | Chemosphere (Oxford) 2003, Vol.50 (2), p.217-222 |
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description | Every two months of 1992, as well as on three occasions in 1994-1995, we obtained leaf samples together with samples of surrounding air from eight well-watered and fertilized sour orange (Citrus aurantium L.) trees that were growing out-of-doors at Phoenix, Arizona, USA. These trees had been planted in the ground as small seedlings in July of 1987 and enclosed in pairs by four clear-plastic-wall open-top chambers of which two have been continuously maintained since November of that year at a CO2 concentration of 400 micromol mol(-1) and two have been maintained at 700 micromol mol(-1). In September 2000, we also extracted north-south and east-west oriented wood cores that passed through the center of each tree's trunk at a height of 45 cm above the ground. Stable-carbon isotope ratios (13C/12C) derived from these leaf, wood and air samples were used to evaluate each tree's intrinsic water-use efficiency (iWUE). The grand-average result was an 80% increase in this important plant parameter in response to the 300 micromol mol(-1) increase in atmospheric CO2 concentration employed in the study. This increase in sour orange tree iWUE is identical to the long-term CO2-induced increase in the trees' production of wood and fruit biomass, which suggests there could be little to no change in total water-use per unit land area for this species as the air's CO2 content continues to rise. It is also identical to the increase in the mean iWUE reported for 23 groups of naturally occurring trees scattered across western North America that was caused by the historical rise in the air's CO2 content that occurred between 1800 and 1985. |
doi_str_mv | 10.1016/S0045-6535(02)00378-8 |
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W ; IDSO, S. B ; KIMBALL, B. A ; BURNS, J. M ; SINHA, A ; STOTT, L</creator><creatorcontrib>LEAVITT, S. W ; IDSO, S. B ; KIMBALL, B. A ; BURNS, J. M ; SINHA, A ; STOTT, L</creatorcontrib><description>Every two months of 1992, as well as on three occasions in 1994-1995, we obtained leaf samples together with samples of surrounding air from eight well-watered and fertilized sour orange (Citrus aurantium L.) trees that were growing out-of-doors at Phoenix, Arizona, USA. These trees had been planted in the ground as small seedlings in July of 1987 and enclosed in pairs by four clear-plastic-wall open-top chambers of which two have been continuously maintained since November of that year at a CO2 concentration of 400 micromol mol(-1) and two have been maintained at 700 micromol mol(-1). In September 2000, we also extracted north-south and east-west oriented wood cores that passed through the center of each tree's trunk at a height of 45 cm above the ground. Stable-carbon isotope ratios (13C/12C) derived from these leaf, wood and air samples were used to evaluate each tree's intrinsic water-use efficiency (iWUE). The grand-average result was an 80% increase in this important plant parameter in response to the 300 micromol mol(-1) increase in atmospheric CO2 concentration employed in the study. This increase in sour orange tree iWUE is identical to the long-term CO2-induced increase in the trees' production of wood and fruit biomass, which suggests there could be little to no change in total water-use per unit land area for this species as the air's CO2 content continues to rise. It is also identical to the increase in the mean iWUE reported for 23 groups of naturally occurring trees scattered across western North America that was caused by the historical rise in the air's CO2 content that occurred between 1800 and 1985.</description><identifier>ISSN: 0045-6535</identifier><identifier>EISSN: 1879-1298</identifier><identifier>DOI: 10.1016/S0045-6535(02)00378-8</identifier><identifier>PMID: 12653293</identifier><identifier>CODEN: CMSHAF</identifier><language>eng</language><publisher>Oxford: Elsevier</publisher><subject>Agricultural and forest climatology and meteorology. Irrigation. Drainage ; Agricultural and forest meteorology ; Agronomy. Soil science and plant productions ; Atmosphere - chemistry ; Biological and medical sciences ; Carbon Dioxide - analysis ; Carbon Dioxide - physiology ; Citrus - growth & development ; Citrus - physiology ; Fundamental and applied biological sciences. Psychology ; General agronomy. 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W</creatorcontrib><creatorcontrib>IDSO, S. B</creatorcontrib><creatorcontrib>KIMBALL, B. A</creatorcontrib><creatorcontrib>BURNS, J. M</creatorcontrib><creatorcontrib>SINHA, A</creatorcontrib><creatorcontrib>STOTT, L</creatorcontrib><title>The effect of long-term atmospheric CO2 enrichment on the intrinsic water-use efficiency of sour orange trees</title><title>Chemosphere (Oxford)</title><addtitle>Chemosphere</addtitle><description>Every two months of 1992, as well as on three occasions in 1994-1995, we obtained leaf samples together with samples of surrounding air from eight well-watered and fertilized sour orange (Citrus aurantium L.) trees that were growing out-of-doors at Phoenix, Arizona, USA. These trees had been planted in the ground as small seedlings in July of 1987 and enclosed in pairs by four clear-plastic-wall open-top chambers of which two have been continuously maintained since November of that year at a CO2 concentration of 400 micromol mol(-1) and two have been maintained at 700 micromol mol(-1). In September 2000, we also extracted north-south and east-west oriented wood cores that passed through the center of each tree's trunk at a height of 45 cm above the ground. Stable-carbon isotope ratios (13C/12C) derived from these leaf, wood and air samples were used to evaluate each tree's intrinsic water-use efficiency (iWUE). The grand-average result was an 80% increase in this important plant parameter in response to the 300 micromol mol(-1) increase in atmospheric CO2 concentration employed in the study. This increase in sour orange tree iWUE is identical to the long-term CO2-induced increase in the trees' production of wood and fruit biomass, which suggests there could be little to no change in total water-use per unit land area for this species as the air's CO2 content continues to rise. It is also identical to the increase in the mean iWUE reported for 23 groups of naturally occurring trees scattered across western North America that was caused by the historical rise in the air's CO2 content that occurred between 1800 and 1985.</description><subject>Agricultural and forest climatology and meteorology. Irrigation. Drainage</subject><subject>Agricultural and forest meteorology</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Atmosphere - chemistry</subject><subject>Biological and medical sciences</subject><subject>Carbon Dioxide - analysis</subject><subject>Carbon Dioxide - physiology</subject><subject>Citrus - growth & development</subject><subject>Citrus - physiology</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>Models, Biological</subject><subject>Plant Leaves - growth & development</subject><subject>Plant Leaves - physiology</subject><subject>Time Factors</subject><subject>Water - physiology</subject><subject>Water balance and requirements. 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Soil science and plant productions</topic><topic>Atmosphere - chemistry</topic><topic>Biological and medical sciences</topic><topic>Carbon Dioxide - analysis</topic><topic>Carbon Dioxide - physiology</topic><topic>Citrus - growth & development</topic><topic>Citrus - physiology</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General agronomy. Plant production</topic><topic>Models, Biological</topic><topic>Plant Leaves - growth & development</topic><topic>Plant Leaves - physiology</topic><topic>Time Factors</topic><topic>Water - physiology</topic><topic>Water balance and requirements. Evapotranspiration</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>LEAVITT, S. W</creatorcontrib><creatorcontrib>IDSO, S. B</creatorcontrib><creatorcontrib>KIMBALL, B. A</creatorcontrib><creatorcontrib>BURNS, J. 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These trees had been planted in the ground as small seedlings in July of 1987 and enclosed in pairs by four clear-plastic-wall open-top chambers of which two have been continuously maintained since November of that year at a CO2 concentration of 400 micromol mol(-1) and two have been maintained at 700 micromol mol(-1). In September 2000, we also extracted north-south and east-west oriented wood cores that passed through the center of each tree's trunk at a height of 45 cm above the ground. Stable-carbon isotope ratios (13C/12C) derived from these leaf, wood and air samples were used to evaluate each tree's intrinsic water-use efficiency (iWUE). The grand-average result was an 80% increase in this important plant parameter in response to the 300 micromol mol(-1) increase in atmospheric CO2 concentration employed in the study. This increase in sour orange tree iWUE is identical to the long-term CO2-induced increase in the trees' production of wood and fruit biomass, which suggests there could be little to no change in total water-use per unit land area for this species as the air's CO2 content continues to rise. It is also identical to the increase in the mean iWUE reported for 23 groups of naturally occurring trees scattered across western North America that was caused by the historical rise in the air's CO2 content that occurred between 1800 and 1985.</abstract><cop>Oxford</cop><pub>Elsevier</pub><pmid>12653293</pmid><doi>10.1016/S0045-6535(02)00378-8</doi><tpages>6</tpages></addata></record> |
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subjects | Agricultural and forest climatology and meteorology. Irrigation. Drainage Agricultural and forest meteorology Agronomy. Soil science and plant productions Atmosphere - chemistry Biological and medical sciences Carbon Dioxide - analysis Carbon Dioxide - physiology Citrus - growth & development Citrus - physiology Fundamental and applied biological sciences. Psychology General agronomy. Plant production Models, Biological Plant Leaves - growth & development Plant Leaves - physiology Time Factors Water - physiology Water balance and requirements. Evapotranspiration |
title | The effect of long-term atmospheric CO2 enrichment on the intrinsic water-use efficiency of sour orange trees |
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