Alkalinization and acidification of stream water with changes in atmospheric deposition in a tropical dry evergreen forest of northeastern Thailand. Issue 4 (4th December 2016)

• Record Type: Journal Article
• Authors: Sase, Hiroyuki; Yamashita, Naoyuki; Luangjame, Jesada; Garivait, Hathairatana; Kietvuttinon, Bopit; Visaratana, Thiti; Kamisako, Masato; Kobayashi, Ryo; Ohta, Seiichi; Shindo, Junko; Hayashi, Kentaro; Toda, Hideshige; Matsuda, Kazuhide
• Is Part Of: Hydrological processes. Volume 31:Issue 4(2017)
• Page Start: 836
• Page End: 846
• Publication Date: 2016-12-04
• Subjects: atmospheric deposition -- chloride -- mineralization -- precipitation -- sulfur -- tropical savanna; Hydrology -- Periodicals; Hydrology -- Research -- Periodicals; Hydrologic models -- Periodicals; Hydrological forecasting -- Periodicals; 631.432
• DOI: 10.1002/hyp.11062
• Languages: English
• ISSNs: 0885-6087

Abstract

Abstract: Field surveys on atmospheric deposition and stream water chemistry were conducted in an evergreen forest in northeastern Thailand characterized by a tropical savanna climate with distinct dry and wet seasons. Atmospheric deposition of ion constituents by throughfall and stemflow was shown to increase in the beginning and end of the wet season, reflecting the precipitation pattern. The pH and electrical conductivity of stream water increased with alkalinity and base cation concentrations due to mineralization of organic matter by the first rain and retention of anions in soil during the start of the wet season. After initial alkalinization, the pH and alkalinity declined rapidly with the highest SO4 2 − concentration displayed in the middle towards the end of the wet season. The magnitude of peaks in SO4 2 − concentration (13.5–60.6 μmolc /L) reflects deposition during the first 2 months of the wet season (March and April) in respective years (60.8–170 molc /ha). Release of SO4 2 − with H +, which is retained in soil during the early wet season, may cause acidification later in the season. The deposition and concentration of SO4 2 − declined over 6 years. However, the pH of stream water declined with increasing concentrations of SO4 2 − and other major ions. The release of materials accumulated in the ecosystem was facilitated by the decrease in SO4 2 − concentration/deposition and increased precipitation in the middle–late wet season. The retention‐release cycle of SO4 2 − largely contributed to both seasonal and interannual variations in stream water chemistry in the tropical savanna climate studied.