Mechanism of nitrate loss from a forested catchment following a small-scale, natural, disturbance

In Matsu-zawa catchment, central Japan, nitrate concentrations in stream water increased following a small-scale, natural disturbance involving an outbreak of pine wilt disease that affected approximately 25% of the forested catchment. To clarify nutrient dynamics in soils and their relationship wit...

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Veröffentlicht in:Canadian journal of forest research 2001-08, Vol.31 (8), p.1326-1335
Hauptverfasser: Hobara, S, Tokuchi, N, Ohte, N, Koba, K, Katsuyama, M, Kim, S.J, Nakanishi, A
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container_end_page 1335
container_issue 8
container_start_page 1326
container_title Canadian journal of forest research
container_volume 31
creator Hobara, S
Tokuchi, N
Ohte, N
Koba, K
Katsuyama, M
Kim, S.J
Nakanishi, A
description In Matsu-zawa catchment, central Japan, nitrate concentrations in stream water increased following a small-scale, natural disturbance involving an outbreak of pine wilt disease that affected approximately 25% of the forested catchment. To clarify nutrient dynamics in soils and their relationship with stream water nitrate, we investigated soil nitrogen dynamics and soil water chemistry in disturbed and undisturbed, water-unsaturated and -saturated plots. The highest values for nitrification rate, nitrate concentration in soil solution, and nitrate exported from the root zone were observed for the disturbed plot. The ratio of nitrification to mineralization in surface soil of the disturbed plot dramatically increased from 1989 (pre-disturbance) to 1997. Root zone leachate from the disturbed area showed gradually increasing ground-water nitrate concentrations in the temporarily saturated zone during lateral, matrix flow. The catchment's deep soils and associated hydrologic processes limited the degree of plant uptake of the nitrate generated in the disturbed area. It was inferred that the persistent high levels of nitrate observed in the stream water resulted largely from the stable high nitrate concentrations observed in the saturated groundwater of this catchment. Stream water nitrate loads discharged following the disturbance were about 16 times greater than prior to it.
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To clarify nutrient dynamics in soils and their relationship with stream water nitrate, we investigated soil nitrogen dynamics and soil water chemistry in disturbed and undisturbed, water-unsaturated and -saturated plots. The highest values for nitrification rate, nitrate concentration in soil solution, and nitrate exported from the root zone were observed for the disturbed plot. The ratio of nitrification to mineralization in surface soil of the disturbed plot dramatically increased from 1989 (pre-disturbance) to 1997. Root zone leachate from the disturbed area showed gradually increasing ground-water nitrate concentrations in the temporarily saturated zone during lateral, matrix flow. The catchment's deep soils and associated hydrologic processes limited the degree of plant uptake of the nitrate generated in the disturbed area. 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General forest ecology ; Japan ; Leachates ; leaching ; losses ; Mineralization ; Moisture content ; mortality ; Nitrates ; Nitrification ; Nutrient dynamics ; outbreaks ; Pinus densiflora ; R&amp;D ; Research &amp; development ; Root zone ; Soil and water pollution ; Soil chemistry ; Soil dynamics ; soil fertility ; Soil science ; Soil solution ; Soil surfaces ; Soil water ; streams ; Synecology ; Terrestrial ecosystems ; Water chemistry ; water quality ; watersheds</subject><ispartof>Canadian journal of forest research, 2001-08, Vol.31 (8), p.1326-1335</ispartof><rights>2002 INIST-CNRS</rights><rights>Copyright National Research Council of Canada Aug 2001</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c413t-7a974317d3aab3f98ab7491493986c5a5666ff467ce3c724e72f92ae275389093</citedby><cites>FETCH-LOGICAL-c413t-7a974317d3aab3f98ab7491493986c5a5666ff467ce3c724e72f92ae275389093</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27903,27904</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=14192059$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Hobara, S</creatorcontrib><creatorcontrib>Tokuchi, N</creatorcontrib><creatorcontrib>Ohte, N</creatorcontrib><creatorcontrib>Koba, K</creatorcontrib><creatorcontrib>Katsuyama, M</creatorcontrib><creatorcontrib>Kim, S.J</creatorcontrib><creatorcontrib>Nakanishi, A</creatorcontrib><title>Mechanism of nitrate loss from a forested catchment following a small-scale, natural, disturbance</title><title>Canadian journal of forest research</title><addtitle>Revue canadienne de recherche forestière</addtitle><description>In Matsu-zawa catchment, central Japan, nitrate concentrations in stream water increased following a small-scale, natural disturbance involving an outbreak of pine wilt disease that affected approximately 25% of the forested catchment. 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To clarify nutrient dynamics in soils and their relationship with stream water nitrate, we investigated soil nitrogen dynamics and soil water chemistry in disturbed and undisturbed, water-unsaturated and -saturated plots. The highest values for nitrification rate, nitrate concentration in soil solution, and nitrate exported from the root zone were observed for the disturbed plot. The ratio of nitrification to mineralization in surface soil of the disturbed plot dramatically increased from 1989 (pre-disturbance) to 1997. Root zone leachate from the disturbed area showed gradually increasing ground-water nitrate concentrations in the temporarily saturated zone during lateral, matrix flow. The catchment's deep soils and associated hydrologic processes limited the degree of plant uptake of the nitrate generated in the disturbed area. It was inferred that the persistent high levels of nitrate observed in the stream water resulted largely from the stable high nitrate concentrations observed in the saturated groundwater of this catchment. Stream water nitrate loads discharged following the disturbance were about 16 times greater than prior to it.</abstract><cop>Ottawa, Canada</cop><pub>NRC Research Press</pub><doi>10.1139/x01-064</doi><tpages>10</tpages></addata></record>
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subjects Agronomy. Soil science and plant productions
Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
Bursaphelenchus xylophilus
Catchments
Chamaecyparis obtusa
disturbed soils
Ecosystems
Forest watersheds
Forestry
Forests
Fresh water ecosystems
Fundamental and applied biological sciences. Psychology
General forest ecology
Generalities. Production, biomass. Quality of wood and forest products. General forest ecology
Japan
Leachates
leaching
losses
Mineralization
Moisture content
mortality
Nitrates
Nitrification
Nutrient dynamics
outbreaks
Pinus densiflora
R&D
Research & development
Root zone
Soil and water pollution
Soil chemistry
Soil dynamics
soil fertility
Soil science
Soil solution
Soil surfaces
Soil water
streams
Synecology
Terrestrial ecosystems
Water chemistry
water quality
watersheds
title Mechanism of nitrate loss from a forested catchment following a small-scale, natural, disturbance
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