The climate in northeastern Thailand is classified as a tropical savanna climate with distinct dry and wet seasons. In accordance with the climate, seasonality of water/material inputs from the atmosphere may largely affect biogeochemical processes in terrestrial ecosystems. In this study, field surveys on atmospheric deposition and stream water chemistry were conducted over 6 years in an evergreen forest of Sakaerat site in northeastern Thailand.
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 (alkalinization) due to mineralization of organic matter by the first rain and retention of anions in the soil during the start of the wet season.
After initial alkalinization, the pH and alkalinity declined rapidly with the highest SO42- concentration displayed in the middle towards the end of the wet season (acidification). The magnitude of peaks in SO42- concentration reflects deposition during the first 2 months of the wet season (March and April) in respective years. Release of SO42- with H+, which is retained in the soil during the early wet season, may cause acidification later in the season.
The deposition and concentration of SO42- declined over 6 years. However, the pH of stream water declined with increasing concentrations of SO42- and other major ions. The release of materials accumulated in the ecosystem was facilitated by the decrease in SO42- concentration/deposition and increased precipitation in the middle–late wet season.
The retention‐release cycle of SO42- largely contributed to both seasonal and inter annual variations in stream water chemistry in the tropical savanna climate studied
The study was supported financially by a Grant‐in‐Aid for Scientific Research on Innovative Areas (20120012) from the Ministry of Education, Culture, Sports, Science, and Technology (MEXT), Japan; the Environment Research and Technology Development Fund (C‐052, C‐082 and B‐0801) from the Ministry of the Environment of Japan; and a grant from the Asia‐Pacific Network for Global Change Research (APN, ARCP2012‐18NMY‐Sase; ARCP2013‐13CMY‐Sase, Sase et al., 2015).The paper on this study is as follows: