Lake Kinneret
Ecology and Management
Book
Chapter
The bathymetry and morphology of Lake Kinneret is influenced by its complex tectonic structure and by high annual sedimentation (~ 100,000 t year−1 for the past 50 years). In general, the lake floor has an asymme...
Chapter
The salinity of Lake Kinneret, which fluctuates between 190 and 280 mg L−1 Cl−, is significantly higher than the salinity of surface streams that flow to the lake. The high salinity is mainly derived from saline ...
Chapter
Following the onset of stratification in spring, the interaction between the oxy-anions of Mo, U, and Sb with reduced solutes in Lake Kinneret lower water mass (LWM) causes the removal of part of these redox-s...
Chapter
The introduction presents a short historical background of the region, including an account of research on Lake Kinneret. An account of recent anthropomorphic changes that have impacted the lake ecosystem and ...
Chapter
This chapter discusses the quantitative aspects of the nitrogen cycle in Lake Kinneret including its sources and sinks. A thorough discussion is devoted to the internal flux of NH4 + from the lowe...
Chapter
The primary source of nitrogen to Lake Kinneret drainage basin is dissolved inorganic N originating in southern Europe and being carried over the Mediterranean Sea by the rain clouds. Evidence is presented tha...
Chapter
Various factors control the seasonal succession of the phytoplankton community in Lake Kinneret. One such factor is whether they are CO2 or HCO3 − users. In spring, CO2-only users such as the dino...
Chapter
This chapter is an overview of the current state of knowledge on Lake Kinneret and the understanding of how this ecosystem functions, as reflected in the chapters of this book.
Chapter
The chapter on the phosphorous (P) cycle of Lake Kinneret presents an overview of more than 40 years of research and monitoring while following up earlier published assessments on P partitioning, sedimentation...
Article
High resolution chemical data collected during summer 2003 indicate that the lower water mass (LWM) of the thermally stratified Lake Kinneret (LK) can be subdivided into three layers: a benthic boundary layer ...
Article
Selenium is an essential micronutrient for the growth of the dinoflagellate Peridinium gatunense that dominates the spring algal bloom in Lake Kinneret (LK). The relationship between the levels of dissolved sele...
Article
Lake Kinneret (Israel) has undergone several prominent chemical and biological changes since 1970. Between 1970 and 1991 significant, long-term gradual increase were recorded in epilimnetic dissolved oxygen (D...