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Hydrological consequences of short rotation forestry; Hydrologiska konsekvenser av energiskogsodling

Abstract

Willow stands on a short rotation basis are introduced in Sweden as an alternative crop for energy purposes. The changes in water balance when growing these stands have been studied by simulations with a mathematical model and by an hydrological object-reference study on a peat bog. The short rotation forests are geographically spread, grown on different soils and with varying management. This gives a spread in water balance results. The studies show that the total evaporation from short rotation forest is higher than from virgin peat land. The total evaporation from a fertilized irrigated stand exceeds the Penman estimate while from an extensively managed stand the total evaporation is less than or equal to the Penman estimate. To reach high production figures a good supply of water is needed. The irrigation should be carefully performed as to avoid production losses or leakage of fertilizers. The changes in runoff is highly dependent on management factors such as drainage and irrigation. When growing short rotation forests the ground water level and the soil water storage decreases during the growth season but is recharged during the winter. The snow storage increases while the frost depth decreases. 11 refs, 12 figs, 2 tabs
Authors:
Persson, Gunn [1] 
  1. Swedish Univ. of Agricultural Sciences, Uppsala (Sweden). Dept. of Soil Sciences
Publication Date:
Dec 31, 1993
Product Type:
Technical Report
Report Number:
NUTEK-EO-93-2; SLU-HY-166
Reference Number:
SCA: 095000; PA: SWD-94:007034; EDB-94:028608; NTS-94:010598; ERA-19:008559; SN: 94001144792
Resource Relation:
Other Information: PBD: [1993]
Subject:
09 BIOMASS FUELS; SHORT ROTATION CULTIVATION; ENVIRONMENTAL EFFECTS; HYDROLOGY; FORESTRY; IRRIGATION; ATMOSPHERIC PRECIPITATIONS; ANNUAL VARIATIONS; GROUND WATER; SIMULATION; 095000; ENVIRONMENTAL ASPECTS
OSTI ID:
10125069
Research Organizations:
Swedish National Board for Industrial and Technical Development (NUTEK), Stockholm (Sweden); Swedish Univ. of Agricultural Sciences, Uppsala (Sweden). Dept. of Soil Sciences
Country of Origin:
Sweden
Language:
Swedish
Other Identifying Numbers:
Other: ON: DE94740263; TRN: SE9407034
Availability:
OSTI; NTIS; INIS
Submitting Site:
SWD
Size:
18 p.
Announcement Date:
Jul 04, 2005

Citation Formats

Persson, Gunn. Hydrological consequences of short rotation forestry; Hydrologiska konsekvenser av energiskogsodling. Sweden: N. p., 1993. Web.
Persson, Gunn. Hydrological consequences of short rotation forestry; Hydrologiska konsekvenser av energiskogsodling. Sweden.
Persson, Gunn. 1993. "Hydrological consequences of short rotation forestry; Hydrologiska konsekvenser av energiskogsodling." Sweden.
@misc{etde_10125069,
title = {Hydrological consequences of short rotation forestry; Hydrologiska konsekvenser av energiskogsodling}
author = {Persson, Gunn}
abstractNote = {Willow stands on a short rotation basis are introduced in Sweden as an alternative crop for energy purposes. The changes in water balance when growing these stands have been studied by simulations with a mathematical model and by an hydrological object-reference study on a peat bog. The short rotation forests are geographically spread, grown on different soils and with varying management. This gives a spread in water balance results. The studies show that the total evaporation from short rotation forest is higher than from virgin peat land. The total evaporation from a fertilized irrigated stand exceeds the Penman estimate while from an extensively managed stand the total evaporation is less than or equal to the Penman estimate. To reach high production figures a good supply of water is needed. The irrigation should be carefully performed as to avoid production losses or leakage of fertilizers. The changes in runoff is highly dependent on management factors such as drainage and irrigation. When growing short rotation forests the ground water level and the soil water storage decreases during the growth season but is recharged during the winter. The snow storage increases while the frost depth decreases. 11 refs, 12 figs, 2 tabs}
place = {Sweden}
year = {1993}
month = {Dec}
}