Interception and Water Recharge Following Afforestation: Experiences from Oak and Norway Spruce Chronosequences in Denmark, Sweden and The Netherlands

Salm, C. van der; Rosenqvist, Lars; Vesterdal, Lars; Hansen, Karin; Gon, H.A.C. Denier van der; Bleeker, A.; Wieggers, Rick; Toorn, A. van den

doi:10.1007/1-4020-4568-9_3

Cited by 5 publications

(2 citation statements)

References 18 publications

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“…The K c value used for forest is relatively high. However, on the basis of investigations by Mossin and Ladekarl [2004] and van der Salm et al [2006] evaporation from the intercepted water is responsible for a relatively high potential evapotranspiration from conifer trees in this area.…”

Section: Methodsmentioning

confidence: 97%

Impact of climate and land use change on the hydrology of a large‐scale agricultural catchment

Roosmalen

Sonnenborg

Jensen

2009

Water Resources Research

140

106

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[1] This paper presents a quantitative comparison of plausible climate and land use change impacts on the hydrology of a large-scale agricultural catchment. An integrated, distributed hydrological model was used to simulate changes in the groundwater system and its discharge to rivers and drains for two climate scenarios (2071-2100). Annual groundwater recharge increased significantly (especially the B2 scenario), giving higher groundwater heads and stream discharges and amplifying the seasonal dynamics significantly. Owing to drier summers, irrigation volumes increased by up to 90% compared to current values. Changing the land use from grass to forest had a minor effect on groundwater recharge, whereas CO 2 effects on transpiration resulted in a relatively large increase in recharge. This study has shown that climate change has the most substantial effect on the hydrology in this catchment, whereas other factors such as irrigation, CO 2 effects on transpiration, and land use changes affect the water balance to a lesser extent.

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Section: Methodsmentioning

confidence: 97%

Impact of climate and land use change on the hydrology of a large‐scale agricultural catchment

Roosmalen

Sonnenborg

Jensen

2009

Water Resources Research

140

106

View full text Add to dashboard Cite

show abstract

“…Apart from measurements of the C pool in the organic layer and mineral soil (up to 25 cm or the bottom of the AP horizon), the carbon pools in above ground biomass and the carbon input by litter fall were measured . Furthermore, data were gathered on the water fluxes ( Van der Salm et al, 2007b) and on the N deposition and N concentrations in soil solution, thus allowing the calculation of N budgets .…”

Section: Chronosequences In Sweden and Denmarkmentioning

confidence: 99%

Modelling soil carbon sequestration of intensively monitored forest plots in Europe by three different approaches

Dijkstra

Reinds

Kros

et al. 2009

Forest Ecology and Management

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Forests

Zerbe¹

2023

Restoration of Ecosystems – Bridging Nature and Humans

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Interception and Water Recharge Following Afforestation: Experiences from Oak and Norway Spruce Chronosequences in Denmark, Sweden and The Netherlands

Cited by 5 publications

References 18 publications

Impact of climate and land use change on the hydrology of a large‐scale agricultural catchment

Impact of climate and land use change on the hydrology of a large‐scale agricultural catchment

Modelling soil carbon sequestration of intensively monitored forest plots in Europe by three different approaches

Forests

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