Effects of historical land use on sediment yield from a lacustrine watershed in central Chile
Identifieur interne : 000C19 ( Main/Exploration ); précédent : 000C18; suivant : 000C20Effects of historical land use on sediment yield from a lacustrine watershed in central Chile
Auteurs : Marco Cisternas [Chili] ; Alberto Araneda [Chili] ; Patricia Martínez [Chili] ; Sergio Pérez [Chili]Source :
- Earth Surface Processes and Landforms [ 0197-9337 ] ; 2001-01.
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- geographic : Chili.
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Abstract
Sediment yield in the San Pedro Lake watershed, inferred from sedimentation in the lake, can be related to land use changes shown on aerial photographs taken during the period 1943–1994. In this watershed, which covers 4·5 km2 of mountainous terrain in San Pedro County, central Chile, the area of native forest species decreased from 70 per cent in 1943 to 13 per cent in 1994. During this same period, the area of pine plantations increased from 4 to 46 per cent. To study effects of these changes, we took a core from the centre of the lake and estimated sedimentation rates by 210Pb dating, which we checked with 137Cs and pine pollen. The results show that sedimentation rate ranged from 5 mg cm−2 a−1 in the late 1800s to 60 mg cm−2 a−1 in the late 1960s. These rates, together with assumptions about the production and delivery of the sediment, give corresponding figures for sediment yields with maximum values close to 1 t ha−1 a−1. Sediment yield between 1955 and 1994 closely tracks the total land use change that can be detected, irrespective of land use type, on sets of aerial photographs taken four to 18 years apart. However, this measure of land use change, while convenient and successful as a predictor of historical erosion, may be unreliable because it probably excludes many changes that occurred in long intervals between successive photographs. Copyright © 2001 John Wiley & Sons, Ltd.
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DOI: 10.1002/1096-9837(200101)26:1<63::AID-ESP157>3.0.CO;2-J
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Landforms</title><idno type="ISSN">0197-9337</idno><idno type="eISSN">1096-9837</idno><imprint><publisher>John Wiley & Sons, Ltd.</publisher><pubPlace>Chichester, UK</pubPlace><date type="published" when="2001-01">2001-01</date><biblScope unit="volume">26</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="63">63</biblScope><biblScope unit="page" to="76">76</biblScope></imprint><idno type="ISSN">0197-9337</idno></series><idno type="istex">2D8DDC799122734D2903BC5593DAF4B1917D2309</idno><idno type="DOI">10.1002/1096-9837(200101)26:1<63::AID-ESP157>3.0.CO;2-J</idno><idno type="ArticleID">ESP157</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0197-9337</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Chile</term><term>GIS</term><term>lake sediments</term><term>land use</term><term>sediment dating</term><term>sediment yield</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Chili</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Sediment yield in the San Pedro Lake watershed, inferred from sedimentation in the lake, can be related to land use changes shown on aerial photographs taken during the period 1943–1994. In this watershed, which covers 4·5 km2 of mountainous terrain in San Pedro County, central Chile, the area of native forest species decreased from 70 per cent in 1943 to 13 per cent in 1994. During this same period, the area of pine plantations increased from 4 to 46 per cent. To study effects of these changes, we took a core from the centre of the lake and estimated sedimentation rates by 210Pb dating, which we checked with 137Cs and pine pollen. The results show that sedimentation rate ranged from 5 mg cm−2 a−1 in the late 1800s to 60 mg cm−2 a−1 in the late 1960s. These rates, together with assumptions about the production and delivery of the sediment, give corresponding figures for sediment yields with maximum values close to 1 t ha−1 a−1. Sediment yield between 1955 and 1994 closely tracks the total land use change that can be detected, irrespective of land use type, on sets of aerial photographs taken four to 18 years apart. However, this measure of land use change, while convenient and successful as a predictor of historical erosion, may be unreliable because it probably excludes many changes that occurred in long intervals between successive photographs. 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