Influence of different drying-rewetting frequencies on available soil nutrients and DOC
To investigate the mechanism of influence of different drying-rewetting frequencies on available soil nutrients and DOC,in this study,we collected cinnamon soil at a depth of 0-10 cm below the surface in Beijing and manipulated soil water stress in the laboratory by exposing soil to 0,1,2,3,or 4 dry...
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description | To investigate the mechanism of influence of different drying-rewetting frequencies on available soil nutrients and DOC,in this study,we collected cinnamon soil at a depth of 0-10 cm below the surface in Beijing and manipulated soil water stress in the laboratory by exposing soil to 0,1,2,3,or 4 drying-rewetting cycles for 58 days,including a 10 day pre-incubation period and a 48 day treatment period. After 58 days,principal soil fertility indexes such as available nutrients and DOC were tested to observe changes as a result of different drying-rewetting frequencies. Data were analyzed using single-factor variance analysis and the Least Significant Difference method( LSD) for the dependent groups. Available K and nitrate nitrogen were lower in the drying and rewetting treatments than in the constantly moist treatment( CM). Low drying-rewetting frequency might lead to the loss of available K,while K release might appear in the late stages of high drying-rewetting frequency conditions. As drying-rewetting frequency increased,the available K also increased. Four drying-rewetting cycles were critical for K release. Increasing the drying-rewetting frequency would result in frequent perturbations to the balance between various forms of nitrogen,and the mineralization rate would increase at the lowest drying-wetting frequency( DW1,1 drying-rewetting cycle) and the highest drying-wetting frequency( DW4,4 drying-rewetting cycles).As drying-wetting frequency increased,nitrate nitrogen of drying-rewetting treatment become closer to that of constantly moist( CM). Soil nitrate nitrogen significantly increased,while available K,ammonium nitrogen,and DOC significantly decreased,with drying-wetting frequency,and available P and p H were relatively insensitive to drying-rewetting frequency.In 48 days,with increase in drying-rewetting frequency( from 1 cycle to 2,3,and 4 cycles) and decrease in dryingrewetting period( from 48 d to 24,16,and 12 d) and the last period of each drying or wetting period( from 24 d to 12,8,and 6 d),nitrate nitrogen and available K tended to increase to levels close to those of the constantly moist condition. |
doi_str_mv | 10.5846/stxb201702190268 |
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After 58 days,principal soil fertility indexes such as available nutrients and DOC were tested to observe changes as a result of different drying-rewetting frequencies. Data were analyzed using single-factor variance analysis and the Least Significant Difference method( LSD) for the dependent groups. Available K and nitrate nitrogen were lower in the drying and rewetting treatments than in the constantly moist treatment( CM). Low drying-rewetting frequency might lead to the loss of available K,while K release might appear in the late stages of high drying-rewetting frequency conditions. As drying-rewetting frequency increased,the available K also increased. Four drying-rewetting cycles were critical for K release. Increasing the drying-rewetting frequency would result in frequent perturbations to the balance between various forms of nitrogen,and the mineralization rate would increase at the lowest drying-wetting frequency( DW1,1 drying-rewetting cycle) and the highest drying-wetting frequency( DW4,4 drying-rewetting cycles).As drying-wetting frequency increased,nitrate nitrogen of drying-rewetting treatment become closer to that of constantly moist( CM). Soil nitrate nitrogen significantly increased,while available K,ammonium nitrogen,and DOC significantly decreased,with drying-wetting frequency,and available P and p H were relatively insensitive to drying-rewetting frequency.In 48 days,with increase in drying-rewetting frequency( from 1 cycle to 2,3,and 4 cycles) and decrease in dryingrewetting period( from 48 d to 24,16,and 12 d) and the last period of each drying or wetting period( from 24 d to 12,8,and 6 d),nitrate nitrogen and available K tended to increase to levels close to those of the constantly moist condition.</description><identifier>ISSN: 1000-0933</identifier><identifier>DOI: 10.5846/stxb201702190268</identifier><language>chi</language><publisher>Beijing: Science Press</publisher><subject>Ammonium ; Data processing ; Dissolved organic carbon ; Drying ; Incubation ; Mineralization ; Moisture content ; Nitrates ; Nitrogen ; Nutrient availability ; Nutrients ; Soil fertility ; Soil investigations ; Soil moisture ; Soil nutrients ; Soil stresses ; Soil water ; Variance analysis ; Water stress ; Wetting</subject><ispartof>Sheng tai xue bao, 2018-01, Vol.38 (5), p.1542</ispartof><rights>Copyright Science Press 2018</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c186t-a70e0703d957f215cd967e93c1d70d43fadd64095d2c05aedd4c4236103a3eb3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Li, Mengxun</creatorcontrib><creatorcontrib>Wang, Dongmei</creatorcontrib><creatorcontrib>Ren, Yuan</creatorcontrib><creatorcontrib>Wang, Xilin</creatorcontrib><title>Influence of different drying-rewetting frequencies on available soil nutrients and DOC</title><title>Sheng tai xue bao</title><description>To investigate the mechanism of influence of different drying-rewetting frequencies on available soil nutrients and DOC,in this study,we collected cinnamon soil at a depth of 0-10 cm below the surface in Beijing and manipulated soil water stress in the laboratory by exposing soil to 0,1,2,3,or 4 drying-rewetting cycles for 58 days,including a 10 day pre-incubation period and a 48 day treatment period. After 58 days,principal soil fertility indexes such as available nutrients and DOC were tested to observe changes as a result of different drying-rewetting frequencies. Data were analyzed using single-factor variance analysis and the Least Significant Difference method( LSD) for the dependent groups. Available K and nitrate nitrogen were lower in the drying and rewetting treatments than in the constantly moist treatment( CM). Low drying-rewetting frequency might lead to the loss of available K,while K release might appear in the late stages of high drying-rewetting frequency conditions. As drying-rewetting frequency increased,the available K also increased. Four drying-rewetting cycles were critical for K release. Increasing the drying-rewetting frequency would result in frequent perturbations to the balance between various forms of nitrogen,and the mineralization rate would increase at the lowest drying-wetting frequency( DW1,1 drying-rewetting cycle) and the highest drying-wetting frequency( DW4,4 drying-rewetting cycles).As drying-wetting frequency increased,nitrate nitrogen of drying-rewetting treatment become closer to that of constantly moist( CM). Soil nitrate nitrogen significantly increased,while available K,ammonium nitrogen,and DOC significantly decreased,with drying-wetting frequency,and available P and p H were relatively insensitive to drying-rewetting frequency.In 48 days,with increase in drying-rewetting frequency( from 1 cycle to 2,3,and 4 cycles) and decrease in dryingrewetting period( from 48 d to 24,16,and 12 d) and the last period of each drying or wetting period( from 24 d to 12,8,and 6 d),nitrate nitrogen and available K tended to increase to levels close to those of the constantly moist condition.</description><subject>Ammonium</subject><subject>Data processing</subject><subject>Dissolved organic carbon</subject><subject>Drying</subject><subject>Incubation</subject><subject>Mineralization</subject><subject>Moisture content</subject><subject>Nitrates</subject><subject>Nitrogen</subject><subject>Nutrient availability</subject><subject>Nutrients</subject><subject>Soil fertility</subject><subject>Soil investigations</subject><subject>Soil moisture</subject><subject>Soil nutrients</subject><subject>Soil stresses</subject><subject>Soil water</subject><subject>Variance analysis</subject><subject>Water stress</subject><subject>Wetting</subject><issn>1000-0933</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNpdkD1PwzAQhj2ARCnsjJaYA2df4tQjKl-VKnWpxBi59hm5Ck6xXaD_nlRlYrobnve908PYjYC7Zlar-1x-NhJEC1JokGp2xiYCACrQiBfsMuctAIJAPWFvi-j7PUVLfPDcBe8pUSzcpUOI71Wibypl3LhP9HnkAmU-RG6-TOjNpieeh9DzuC8pjLnMTXT8cTW_Yufe9Jmu_-aUrZ-f1vPXarl6WcwflpUVM1Uq0wJBC-h003opGuu0akmjFa4FV6M3zqkadOOkhcaQc7WtJSoBaJA2OGW3p9pdGsb3cum2wz7F8WInhUAFWKMeKThRNg05J_LdLoUPkw6dgO5orPtvDH8B_HVh2g</recordid><startdate>20180101</startdate><enddate>20180101</enddate><creator>Li, Mengxun</creator><creator>Wang, Dongmei</creator><creator>Ren, Yuan</creator><creator>Wang, Xilin</creator><general>Science Press</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7ST</scope><scope>7UA</scope><scope>C1K</scope><scope>SOI</scope></search><sort><creationdate>20180101</creationdate><title>Influence of different drying-rewetting frequencies on available soil nutrients and DOC</title><author>Li, Mengxun ; Wang, Dongmei ; Ren, Yuan ; Wang, Xilin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c186t-a70e0703d957f215cd967e93c1d70d43fadd64095d2c05aedd4c4236103a3eb3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi</language><creationdate>2018</creationdate><topic>Ammonium</topic><topic>Data processing</topic><topic>Dissolved organic carbon</topic><topic>Drying</topic><topic>Incubation</topic><topic>Mineralization</topic><topic>Moisture content</topic><topic>Nitrates</topic><topic>Nitrogen</topic><topic>Nutrient availability</topic><topic>Nutrients</topic><topic>Soil fertility</topic><topic>Soil investigations</topic><topic>Soil moisture</topic><topic>Soil nutrients</topic><topic>Soil stresses</topic><topic>Soil water</topic><topic>Variance analysis</topic><topic>Water stress</topic><topic>Wetting</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Li, Mengxun</creatorcontrib><creatorcontrib>Wang, Dongmei</creatorcontrib><creatorcontrib>Ren, Yuan</creatorcontrib><creatorcontrib>Wang, Xilin</creatorcontrib><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Environment Abstracts</collection><jtitle>Sheng tai xue bao</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Li, Mengxun</au><au>Wang, Dongmei</au><au>Ren, Yuan</au><au>Wang, Xilin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Influence of different drying-rewetting frequencies on available soil nutrients and DOC</atitle><jtitle>Sheng tai xue bao</jtitle><date>2018-01-01</date><risdate>2018</risdate><volume>38</volume><issue>5</issue><spage>1542</spage><pages>1542-</pages><issn>1000-0933</issn><abstract>To investigate the mechanism of influence of different drying-rewetting frequencies on available soil nutrients and DOC,in this study,we collected cinnamon soil at a depth of 0-10 cm below the surface in Beijing and manipulated soil water stress in the laboratory by exposing soil to 0,1,2,3,or 4 drying-rewetting cycles for 58 days,including a 10 day pre-incubation period and a 48 day treatment period. After 58 days,principal soil fertility indexes such as available nutrients and DOC were tested to observe changes as a result of different drying-rewetting frequencies. Data were analyzed using single-factor variance analysis and the Least Significant Difference method( LSD) for the dependent groups. Available K and nitrate nitrogen were lower in the drying and rewetting treatments than in the constantly moist treatment( CM). Low drying-rewetting frequency might lead to the loss of available K,while K release might appear in the late stages of high drying-rewetting frequency conditions. As drying-rewetting frequency increased,the available K also increased. Four drying-rewetting cycles were critical for K release. Increasing the drying-rewetting frequency would result in frequent perturbations to the balance between various forms of nitrogen,and the mineralization rate would increase at the lowest drying-wetting frequency( DW1,1 drying-rewetting cycle) and the highest drying-wetting frequency( DW4,4 drying-rewetting cycles).As drying-wetting frequency increased,nitrate nitrogen of drying-rewetting treatment become closer to that of constantly moist( CM). Soil nitrate nitrogen significantly increased,while available K,ammonium nitrogen,and DOC significantly decreased,with drying-wetting frequency,and available P and p H were relatively insensitive to drying-rewetting frequency.In 48 days,with increase in drying-rewetting frequency( from 1 cycle to 2,3,and 4 cycles) and decrease in dryingrewetting period( from 48 d to 24,16,and 12 d) and the last period of each drying or wetting period( from 24 d to 12,8,and 6 d),nitrate nitrogen and available K tended to increase to levels close to those of the constantly moist condition.</abstract><cop>Beijing</cop><pub>Science Press</pub><doi>10.5846/stxb201702190268</doi></addata></record> |
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subjects | Ammonium Data processing Dissolved organic carbon Drying Incubation Mineralization Moisture content Nitrates Nitrogen Nutrient availability Nutrients Soil fertility Soil investigations Soil moisture Soil nutrients Soil stresses Soil water Variance analysis Water stress Wetting |
title | Influence of different drying-rewetting frequencies on available soil nutrients and DOC |
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