Home > Research > Publications & Outputs > The Influence of Trees on Soil Hydraulic Proper...

Electronic data

  • 11003579.pdf

    Final published version, 5.66 MB, PDF document

    Available under license: CC BY-ND

View graph of relations

The Influence of Trees on Soil Hydraulic Properties : Species Effects and the Provision of Ecosystem Services.

Research output: ThesisDoctoral Thesis

Unpublished

Standard

The Influence of Trees on Soil Hydraulic Properties : Species Effects and the Provision of Ecosystem Services. / Chandler, Kathryn Ruth.
Lancaster: Lancaster University, 2014. 123 p.

Research output: ThesisDoctoral Thesis

Harvard

APA

Vancouver

Author

Bibtex

@phdthesis{1397c5053776459fba2f010ff7295e63,
title = "The Influence of Trees on Soil Hydraulic Properties : Species Effects and the Provision of Ecosystem Services.",
abstract = "Trees contribute to a number of important ecosystem services through their influence on soil properties and functions, including water purification and regulation. Forest soils tend to have a higher saturated hydraulic conductivity (Ks) than soils under other vegetation, so the establishment of streamside tree buffer zones and strategically planted woodland is increasingly being promoted to reduce or intercept surface runoff from agricultural and urban environments that may contribute to diffuse pollution and flooding. Despite this, our understanding of how trees affect soil hydraulic properties is still extremely limited. The main aims of the work outlined in this thesis were to compare the effect of a broadleaf (sycamore) and a conifer (Scots pine) tree on Ks to determine if this differs between species type, to examine the effect of land use on Ks under forest cover and to investigate the key underlying mechanisms involved. Results showed significantly higher Ks under undisturbed mature Scots pine forest compared with sycamore forest, indicating a species effect. Forest soils also had significantly higher Ks than pasture grazed by sheep; however, when sheep were grazed under forest cover, there was no significant difference between forest and pasture, suggesting that the effect of land use masked the effect of trees on Ks. An investigation of soil flow pathways and pore characteristics showed that significantly higher Ks corresponded with significantly higher soil macroporosity and macropore flow. A mesocosm experiment, undertaken to investigate the influence of tree roots and associated soil macrofauna on Ks, was found to be of insufficient duration for significant changes to occur; however non-significant higher Ks observed under Scots pine compared with sycamore were consistent with the study of more mature trees. The results of a glasshouse experiment investigating the influence of leaf litter on Ks showed that leaf litter had a negative effect and litter type had more of an effect than litter quantity.",
keywords = "MiAaPQ, Environmental management.",
author = "Chandler, {Kathryn Ruth}",
note = "Thesis (Ph.D.)--Lancaster University (United Kingdom), 2014.",
year = "2014",
language = "English",
publisher = "Lancaster University",
school = "Lancaster University",

}

RIS

TY - BOOK

T1 - The Influence of Trees on Soil Hydraulic Properties : Species Effects and the Provision of Ecosystem Services.

AU - Chandler, Kathryn Ruth

N1 - Thesis (Ph.D.)--Lancaster University (United Kingdom), 2014.

PY - 2014

Y1 - 2014

N2 - Trees contribute to a number of important ecosystem services through their influence on soil properties and functions, including water purification and regulation. Forest soils tend to have a higher saturated hydraulic conductivity (Ks) than soils under other vegetation, so the establishment of streamside tree buffer zones and strategically planted woodland is increasingly being promoted to reduce or intercept surface runoff from agricultural and urban environments that may contribute to diffuse pollution and flooding. Despite this, our understanding of how trees affect soil hydraulic properties is still extremely limited. The main aims of the work outlined in this thesis were to compare the effect of a broadleaf (sycamore) and a conifer (Scots pine) tree on Ks to determine if this differs between species type, to examine the effect of land use on Ks under forest cover and to investigate the key underlying mechanisms involved. Results showed significantly higher Ks under undisturbed mature Scots pine forest compared with sycamore forest, indicating a species effect. Forest soils also had significantly higher Ks than pasture grazed by sheep; however, when sheep were grazed under forest cover, there was no significant difference between forest and pasture, suggesting that the effect of land use masked the effect of trees on Ks. An investigation of soil flow pathways and pore characteristics showed that significantly higher Ks corresponded with significantly higher soil macroporosity and macropore flow. A mesocosm experiment, undertaken to investigate the influence of tree roots and associated soil macrofauna on Ks, was found to be of insufficient duration for significant changes to occur; however non-significant higher Ks observed under Scots pine compared with sycamore were consistent with the study of more mature trees. The results of a glasshouse experiment investigating the influence of leaf litter on Ks showed that leaf litter had a negative effect and litter type had more of an effect than litter quantity.

AB - Trees contribute to a number of important ecosystem services through their influence on soil properties and functions, including water purification and regulation. Forest soils tend to have a higher saturated hydraulic conductivity (Ks) than soils under other vegetation, so the establishment of streamside tree buffer zones and strategically planted woodland is increasingly being promoted to reduce or intercept surface runoff from agricultural and urban environments that may contribute to diffuse pollution and flooding. Despite this, our understanding of how trees affect soil hydraulic properties is still extremely limited. The main aims of the work outlined in this thesis were to compare the effect of a broadleaf (sycamore) and a conifer (Scots pine) tree on Ks to determine if this differs between species type, to examine the effect of land use on Ks under forest cover and to investigate the key underlying mechanisms involved. Results showed significantly higher Ks under undisturbed mature Scots pine forest compared with sycamore forest, indicating a species effect. Forest soils also had significantly higher Ks than pasture grazed by sheep; however, when sheep were grazed under forest cover, there was no significant difference between forest and pasture, suggesting that the effect of land use masked the effect of trees on Ks. An investigation of soil flow pathways and pore characteristics showed that significantly higher Ks corresponded with significantly higher soil macroporosity and macropore flow. A mesocosm experiment, undertaken to investigate the influence of tree roots and associated soil macrofauna on Ks, was found to be of insufficient duration for significant changes to occur; however non-significant higher Ks observed under Scots pine compared with sycamore were consistent with the study of more mature trees. The results of a glasshouse experiment investigating the influence of leaf litter on Ks showed that leaf litter had a negative effect and litter type had more of an effect than litter quantity.

KW - MiAaPQ

KW - Environmental management.

M3 - Doctoral Thesis

PB - Lancaster University

CY - Lancaster

ER -