Stemflow variation in Mexico’s northeastern forest communities: Its contribution to soil moisture content and aquifer recharge
► A comprehensive stemflow dataset was collected for two Mexico’s northern plant communities. ► For each species and for each stand, stemflow coefficients and infiltration depths are reported. ► Statistical stemflow differences are found between the species, plant communities and stands. ► Stemflow...
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| description | ► A comprehensive stemflow dataset was collected for two Mexico’s northern plant communities. ► For each species and for each stand, stemflow coefficients and infiltration depths are reported. ► Statistical stemflow differences are found between the species, plant communities and stands. ► Stemflow extrapolated threefold from trees to stands because of overstocked forests. ► Temperate forest stemflow appears to contribute to aquifer recharge because of shallow soils.
Stemflow hydro-ecological importance was measured in trees and assessed in Mexico’s northeast forest stands by answering three basic questions: (a) what are the intra and inter-specific stemflow variations; (b) is the stemflow coefficient constant from tree level to stand scales? and (c) what is the stemflow area and wetted soil volume in individual trees and the stemflow volume discharged at the stand scale in two plant communities of northeastern Mexico? Gross rainfall and stemflow flux measurements were conducted on 78 trees of semi-arid, sub-tropical (31
Diospyros texana; 14
Acacia rigidula; four
Bumelia celastrina; five
Condalia hookeri; three
Cordia bioissieri; three
Pithecellobium pallens) and temperate forest communities (six
Pinus pseudostrobus Lindl. and 12
Quercus spp.). Stemflow was extrapolated from individual trees to the stand scale using 98 inventory plots (1600
m
2
ha
−1 each) placed in oak–pine forests and 37 quadrats (5
m
×
5
m each) distributed across the Tamaulipan thornscrub forest range. Stemflow infiltration flux and infiltration area measurements assessed the wetted soil volume. Daily measurements were conducted from May of 1997 to November of 1998. Results showed that stemflow coefficients varied between plant communities since they averaged (confidence intervals,
α
=
0.05) 2.49% (0.57), 0.30% (0.09), and 0.77% (0.27) of the bulk precipitation for Tamaulipan thornscrub, pine, and oak forests, respectively. Intra-specific stemflow variations could not be identified in Tamaulipan although in temperate tree species. Basal diameter explained intra-specific stemflow variation in both plant communities. Stemflow increased threefold since it accounted for by 6.38% and 2.19% of the total bulk rainfall for Tamaulipan thornscrub quadrats and temperate oak–pine inventory plots, respectively. Small shrubs growing underneath large trees, in combination with the presence of small-diameter trees that recorded the largest stemflow coefficients appear to explain the increase of the st |
| doi_str_mv | 10.1016/j.jhydrol.2011.07.006 |
| format | Article |
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Stemflow hydro-ecological importance was measured in trees and assessed in Mexico’s northeast forest stands by answering three basic questions: (a) what are the intra and inter-specific stemflow variations; (b) is the stemflow coefficient constant from tree level to stand scales? and (c) what is the stemflow area and wetted soil volume in individual trees and the stemflow volume discharged at the stand scale in two plant communities of northeastern Mexico? Gross rainfall and stemflow flux measurements were conducted on 78 trees of semi-arid, sub-tropical (31
Diospyros texana; 14
Acacia rigidula; four
Bumelia celastrina; five
Condalia hookeri; three
Cordia bioissieri; three
Pithecellobium pallens) and temperate forest communities (six
Pinus pseudostrobus Lindl. and 12
Quercus spp.). Stemflow was extrapolated from individual trees to the stand scale using 98 inventory plots (1600
m
2
ha
−1 each) placed in oak–pine forests and 37 quadrats (5
m
×
5
m each) distributed across the Tamaulipan thornscrub forest range. Stemflow infiltration flux and infiltration area measurements assessed the wetted soil volume. Daily measurements were conducted from May of 1997 to November of 1998. Results showed that stemflow coefficients varied between plant communities since they averaged (confidence intervals,
α
=
0.05) 2.49% (0.57), 0.30% (0.09), and 0.77% (0.27) of the bulk precipitation for Tamaulipan thornscrub, pine, and oak forests, respectively. Intra-specific stemflow variations could not be identified in Tamaulipan although in temperate tree species. Basal diameter explained intra-specific stemflow variation in both plant communities. Stemflow increased threefold since it accounted for by 6.38% and 2.19% of the total bulk rainfall for Tamaulipan thornscrub quadrats and temperate oak–pine inventory plots, respectively. Small shrubs growing underneath large trees, in combination with the presence of small-diameter trees that recorded the largest stemflow coefficients appear to explain the increase of the stemflow coefficient from trees to stands. Stemflow replenishes soil moisture on the average 4.5 (1.4) times larger than does incident rainfall in open soils and appear to contribute to aquifer recharge in temperate forests due to a combination of shallow soils, high infiltration fluxes and the stemflow volume generated during rainfalls with depths >15
mm. Tracing studies should be conducted to test the hypothesis of the stemflow contribution to aquifer recharge in temperate forests of northeastern Mexico.</description><identifier>ISSN: 0022-1694</identifier><identifier>EISSN: 1879-2707</identifier><identifier>DOI: 10.1016/j.jhydrol.2011.07.006</identifier><identifier>CODEN: JHYDA7</identifier><language>eng</language><publisher>Kidlington: Elsevier B.V</publisher><subject>Acacia rigidula ; Animal and plant ecology ; Animal, plant and microbial ecology ; Aquifer recharge ; Biological and medical sciences ; Bumelia celastrina ; Coefficients ; Communities ; Condalia hookeri ; Cordia ; Diospyros texana ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Forests ; Fundamental and applied biological sciences. Psychology ; Hydrogeology ; Hydrology ; Hydrology. Hydrogeology ; Intra and interspecific variation ; Pinus ; Pithecellobium pallens ; Quercus ; Rainfall ; Soil (material) ; Stands ; Stemflow volume and coefficient ; Supports ; Synecology ; Terrestrial ecosystems ; Tree and stand scales ; Trees</subject><ispartof>Journal of hydrology (Amsterdam), 2011-09, Vol.408 (1), p.35-42</ispartof><rights>2011 Elsevier B.V.</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a493t-6912e1a2e831c97b3bf6ed47b4854ad7971fdbb65c010862190114367ee5dca3</citedby><cites>FETCH-LOGICAL-a493t-6912e1a2e831c97b3bf6ed47b4854ad7971fdbb65c010862190114367ee5dca3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.jhydrol.2011.07.006$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=24559344$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>NAVAR, José</creatorcontrib><title>Stemflow variation in Mexico’s northeastern forest communities: Its contribution to soil moisture content and aquifer recharge</title><title>Journal of hydrology (Amsterdam)</title><description>► A comprehensive stemflow dataset was collected for two Mexico’s northern plant communities. ► For each species and for each stand, stemflow coefficients and infiltration depths are reported. ► Statistical stemflow differences are found between the species, plant communities and stands. ► Stemflow extrapolated threefold from trees to stands because of overstocked forests. ► Temperate forest stemflow appears to contribute to aquifer recharge because of shallow soils.
Stemflow hydro-ecological importance was measured in trees and assessed in Mexico’s northeast forest stands by answering three basic questions: (a) what are the intra and inter-specific stemflow variations; (b) is the stemflow coefficient constant from tree level to stand scales? and (c) what is the stemflow area and wetted soil volume in individual trees and the stemflow volume discharged at the stand scale in two plant communities of northeastern Mexico? Gross rainfall and stemflow flux measurements were conducted on 78 trees of semi-arid, sub-tropical (31
Diospyros texana; 14
Acacia rigidula; four
Bumelia celastrina; five
Condalia hookeri; three
Cordia bioissieri; three
Pithecellobium pallens) and temperate forest communities (six
Pinus pseudostrobus Lindl. and 12
Quercus spp.). Stemflow was extrapolated from individual trees to the stand scale using 98 inventory plots (1600
m
2
ha
−1 each) placed in oak–pine forests and 37 quadrats (5
m
×
5
m each) distributed across the Tamaulipan thornscrub forest range. Stemflow infiltration flux and infiltration area measurements assessed the wetted soil volume. Daily measurements were conducted from May of 1997 to November of 1998. Results showed that stemflow coefficients varied between plant communities since they averaged (confidence intervals,
α
=
0.05) 2.49% (0.57), 0.30% (0.09), and 0.77% (0.27) of the bulk precipitation for Tamaulipan thornscrub, pine, and oak forests, respectively. Intra-specific stemflow variations could not be identified in Tamaulipan although in temperate tree species. Basal diameter explained intra-specific stemflow variation in both plant communities. Stemflow increased threefold since it accounted for by 6.38% and 2.19% of the total bulk rainfall for Tamaulipan thornscrub quadrats and temperate oak–pine inventory plots, respectively. Small shrubs growing underneath large trees, in combination with the presence of small-diameter trees that recorded the largest stemflow coefficients appear to explain the increase of the stemflow coefficient from trees to stands. Stemflow replenishes soil moisture on the average 4.5 (1.4) times larger than does incident rainfall in open soils and appear to contribute to aquifer recharge in temperate forests due to a combination of shallow soils, high infiltration fluxes and the stemflow volume generated during rainfalls with depths >15
mm. Tracing studies should be conducted to test the hypothesis of the stemflow contribution to aquifer recharge in temperate forests of northeastern Mexico.</description><subject>Acacia rigidula</subject><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Aquifer recharge</subject><subject>Biological and medical sciences</subject><subject>Bumelia celastrina</subject><subject>Coefficients</subject><subject>Communities</subject><subject>Condalia hookeri</subject><subject>Cordia</subject><subject>Diospyros texana</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Forests</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Hydrogeology</subject><subject>Hydrology</subject><subject>Hydrology. Hydrogeology</subject><subject>Intra and interspecific variation</subject><subject>Pinus</subject><subject>Pithecellobium pallens</subject><subject>Quercus</subject><subject>Rainfall</subject><subject>Soil (material)</subject><subject>Stands</subject><subject>Stemflow volume and coefficient</subject><subject>Supports</subject><subject>Synecology</subject><subject>Terrestrial ecosystems</subject><subject>Tree and stand scales</subject><subject>Trees</subject><issn>0022-1694</issn><issn>1879-2707</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNqFkcFO3DAQhq2qSN1CH6GSL4hektqOY8dcqgoVigTqodwtx5mwXiU22A6UG6_R1-NJMOyqx-LLSJ7vn9H8P0KfKakpoeLrpt6sH4YYppoRSmsia0LEO7SinVQVk0S-RytCGKuoUPwD-pjShpTXNHyFHn9nmMcp3OM7E53JLnjsPL6EP86Gp8e_CfsQ8xpMyhA9HkOElLEN87x4lx2kY3yeU_nwObp-edXngFNwE56DS3mJ8NoFn7HxAza3ixsh4gh2beI1HKC90UwJPu3qPro6_XF18rO6-HV2fvL9ojJcNbkSijKghkHXUKtk3_SjgIHLnnctN4NUko5D34vWEko6wagqVvBGSIB2sKbZR0fbsTcx3C7lBj27ZGGajIewJN0pRQVjLSnkl_-SVMgyuFOsLWi7RW0MKUUY9U10s4kPmhL9Eo3e6F00-iUaTaQu0RTd4W6FSdZMYzTeuvRPzHjbqobzwn3bclCMuXMQdbIOvIXBFfuyHoJ7Y9MzSuCq_w</recordid><startdate>20110930</startdate><enddate>20110930</enddate><creator>NAVAR, José</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>SOI</scope></search><sort><creationdate>20110930</creationdate><title>Stemflow variation in Mexico’s northeastern forest communities: Its contribution to soil moisture content and aquifer recharge</title><author>NAVAR, José</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a493t-6912e1a2e831c97b3bf6ed47b4854ad7971fdbb65c010862190114367ee5dca3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Acacia rigidula</topic><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>Aquifer recharge</topic><topic>Biological and medical sciences</topic><topic>Bumelia celastrina</topic><topic>Coefficients</topic><topic>Communities</topic><topic>Condalia hookeri</topic><topic>Cordia</topic><topic>Diospyros texana</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Forests</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Hydrogeology</topic><topic>Hydrology</topic><topic>Hydrology. Hydrogeology</topic><topic>Intra and interspecific variation</topic><topic>Pinus</topic><topic>Pithecellobium pallens</topic><topic>Quercus</topic><topic>Rainfall</topic><topic>Soil (material)</topic><topic>Stands</topic><topic>Stemflow volume and coefficient</topic><topic>Supports</topic><topic>Synecology</topic><topic>Terrestrial ecosystems</topic><topic>Tree and stand scales</topic><topic>Trees</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>NAVAR, José</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Journal of hydrology (Amsterdam)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>NAVAR, José</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Stemflow variation in Mexico’s northeastern forest communities: Its contribution to soil moisture content and aquifer recharge</atitle><jtitle>Journal of hydrology (Amsterdam)</jtitle><date>2011-09-30</date><risdate>2011</risdate><volume>408</volume><issue>1</issue><spage>35</spage><epage>42</epage><pages>35-42</pages><issn>0022-1694</issn><eissn>1879-2707</eissn><coden>JHYDA7</coden><abstract>► A comprehensive stemflow dataset was collected for two Mexico’s northern plant communities. ► For each species and for each stand, stemflow coefficients and infiltration depths are reported. ► Statistical stemflow differences are found between the species, plant communities and stands. ► Stemflow extrapolated threefold from trees to stands because of overstocked forests. ► Temperate forest stemflow appears to contribute to aquifer recharge because of shallow soils.
Stemflow hydro-ecological importance was measured in trees and assessed in Mexico’s northeast forest stands by answering three basic questions: (a) what are the intra and inter-specific stemflow variations; (b) is the stemflow coefficient constant from tree level to stand scales? and (c) what is the stemflow area and wetted soil volume in individual trees and the stemflow volume discharged at the stand scale in two plant communities of northeastern Mexico? Gross rainfall and stemflow flux measurements were conducted on 78 trees of semi-arid, sub-tropical (31
Diospyros texana; 14
Acacia rigidula; four
Bumelia celastrina; five
Condalia hookeri; three
Cordia bioissieri; three
Pithecellobium pallens) and temperate forest communities (six
Pinus pseudostrobus Lindl. and 12
Quercus spp.). Stemflow was extrapolated from individual trees to the stand scale using 98 inventory plots (1600
m
2
ha
−1 each) placed in oak–pine forests and 37 quadrats (5
m
×
5
m each) distributed across the Tamaulipan thornscrub forest range. Stemflow infiltration flux and infiltration area measurements assessed the wetted soil volume. Daily measurements were conducted from May of 1997 to November of 1998. Results showed that stemflow coefficients varied between plant communities since they averaged (confidence intervals,
α
=
0.05) 2.49% (0.57), 0.30% (0.09), and 0.77% (0.27) of the bulk precipitation for Tamaulipan thornscrub, pine, and oak forests, respectively. Intra-specific stemflow variations could not be identified in Tamaulipan although in temperate tree species. Basal diameter explained intra-specific stemflow variation in both plant communities. Stemflow increased threefold since it accounted for by 6.38% and 2.19% of the total bulk rainfall for Tamaulipan thornscrub quadrats and temperate oak–pine inventory plots, respectively. Small shrubs growing underneath large trees, in combination with the presence of small-diameter trees that recorded the largest stemflow coefficients appear to explain the increase of the stemflow coefficient from trees to stands. Stemflow replenishes soil moisture on the average 4.5 (1.4) times larger than does incident rainfall in open soils and appear to contribute to aquifer recharge in temperate forests due to a combination of shallow soils, high infiltration fluxes and the stemflow volume generated during rainfalls with depths >15
mm. Tracing studies should be conducted to test the hypothesis of the stemflow contribution to aquifer recharge in temperate forests of northeastern Mexico.</abstract><cop>Kidlington</cop><pub>Elsevier B.V</pub><doi>10.1016/j.jhydrol.2011.07.006</doi><tpages>8</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0022-1694 |
| ispartof | Journal of hydrology (Amsterdam), 2011-09, Vol.408 (1), p.35-42 |
| issn | 0022-1694 1879-2707 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_899162250 |
| source | Elsevier ScienceDirect Journals Complete |
| subjects | Acacia rigidula Animal and plant ecology Animal, plant and microbial ecology Aquifer recharge Biological and medical sciences Bumelia celastrina Coefficients Communities Condalia hookeri Cordia Diospyros texana Earth sciences Earth, ocean, space Exact sciences and technology Forests Fundamental and applied biological sciences. Psychology Hydrogeology Hydrology Hydrology. Hydrogeology Intra and interspecific variation Pinus Pithecellobium pallens Quercus Rainfall Soil (material) Stands Stemflow volume and coefficient Supports Synecology Terrestrial ecosystems Tree and stand scales Trees |
| title | Stemflow variation in Mexico’s northeastern forest communities: Its contribution to soil moisture content and aquifer recharge |
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