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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Published in | Journal of hydrology (Amsterdam) Vol. 408; no. 1; pp. 35 - 42 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Kidlington
Elsevier B.V
30.09.2011
Elsevier |
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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. |
---|---|
AbstractList | 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 (1600m2ha-1 each) placed in oak-pine forests and 37 quadrats (5m5m 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, alpha =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 >15mm. Tracing studies should be conducted to test the hypothesis of the stemflow contribution to aquifer recharge in temperate forests of northeastern Mexico. ► 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. |
Author | Návar, José |
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Keywords | Stemflow volume and coefficient Intra and interspecific variation Aquifer recharge Tree and stand scales ground water ground-water recharge Pinus inventory North America trees Pinaceae aquifers Dicotyledoneae soils rainfall soil moisture atmospheric precipitation gymnosperms Plantae forests infiltration depth Quercus angiosperms Coniferales Spermatophyta vegetation effects confidence interval |
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Snippet | ► A comprehensive stemflow dataset was collected for two Mexico’s northern plant communities. ► For each species and for each stand, stemflow coefficients and... Stemflow hydro-ecological importance was measured in trees and assessed in Mexico's northeast forest stands by answering three basic questions: (a) what are... |
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SubjectTerms | 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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