Abstract

The vertical and diurnal variation of nitrogen and phosphorus forms, as well as that of soluble reactive silica (SRS), were studied in four sampling days at Gar9as reservoir, a shallow tropical one located in the city of São Paulo, in southeastern Brazil. Except for N-NH4, all other inorganic forms of nitrogen (N-NO2, N-NO3, and total N) demonstrated decreased concentrations toward the bottom of reservoir. Similarly, all showed significant diurnal differences on every sampling day, with increased values during the night due to absence of photosynthetic assimilation during that period. In the sampling days, these forms decreased on the spring sampling day due to the bloom of Microcystis registered during this period of the year. All three forms of phosphorus (SRP, particulate P, and total P) showed significant vertical variation, except on the fall sampling day. On the summer sampling day there was an increase of both total P and particulate P, the latter because it constitutes more than 70% of the total P during all sampling days. Hourly phosphorus variation was significant during all sampling days, except for the summer one. The SRS vertical variation was significant during all sampling days, except for that in the spring. It was also different hourly on sampling days.

Highlights

  • Surface waters in contact with the atmospheric mixture of gases and water vapor will absorb some of its components

  • Results of ANOVA performed to establish the significance of vertical variation of N-NO3, N-NO2, and total N on each sampling day at Garças reservoir

  • Considering the four sampling days (Fig. 6), different nitrogen forms showed marked decreases on the spring sampling day, most possibly related to the Microcystis bloom occurring at that time

Read more

Summary

Introduction

Surface waters in contact with the atmospheric mixture of gases and water vapor will absorb some of its components. Oxygen, and carbon dioxide are especially important because of their very essential biological roles. Oxygen is one of the most abundant constituents of the atmosphere Despite CO in the air being 2 surpassed some 28 times in abundance by argon, for example, it is at least 15 times more soluble in water than the two most abundant atmospheric gases (N and O ) (Wetzel, 1993; Cole, 1983). Water mixing is very important for CO 2 availability to phytoplankton, especially the nonmotile forms for which a gradient of the gas is established in their immediate surroundings.

Objectives
Methods
Results
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.