Toxicity of major cations and anions (Na+, K+, Ca2+, Cl-, and SO4(2-)) to a macrophyte and an alga.

In many freshwater systems around the world, the concentrations of major ions (Na(+), K(+), Ca(2+), Mg(2+), Cl(-), HCO(3)(-), CO(3)(2-), and SO(4)(2-)) are exhibiting increasing trends, approaching the concentrations historically found mainly in estuaries. The objectives of the present study were to determine at what concentrations these salts are toxic to an aquatic plant and a green alga, to investigate two potential mechanisms of toxicity, and to determine the usefulness of conductivity as an indicator of salt toxicity. In a series of laboratory trials, Lemna minor and Pseudokirchneriella subcapitata were exposed to a range of concentrations of five different salts. Conductivity levels that caused 10 or 50% reductions in growth-related traits (EC10 and EC50, respectively) were determined, using conductivity of the test solutions as the independent variable. The EC10 values ranged from 0.44 to 2.67 mS/cm for P. subcapitata and from 1.3 to >19 mS/cm for L. minor. The EC50 values ranged from 1.7 to 5.8 mS/cm for P. subcapitata and from 4.2 to >27 mS/cm for L. minor. For both species the EC values varied dramatically among the salts. Pseudokirchneriella subcapitata was most sensitive to KCl and NaCl, whereas L. minor was most sensitive to Na(2)SO(4). The mechanism of toxicity does not appear to be related to production of reactive oxygen species, nor to reduction in chlorophyll concentrations. Because toxicity was strongly influenced by salt composition, regulation and management of specific ions may be preferable to conductivity.

Forest to reclaimed mine land use change leads to altered ecosystem structure and function.

The United States' use of coal results in many environmental alterations. In the Appalachian coal belt region, one widespread alteration is conversion of forest to reclaimed mineland. The goal of this study was to quantify the changes to ecosystem structure and function associated with a conversion from forest to reclaimed mine grassland by comparing a small watershed containing a 15-year-old reclaimed mine with a forested, reference watershed in western Maryland. Major differences were apparent between the two watersheds in terms of biogeochemistry. Total C, N, and P pools were all substantially lower at the mined site, mainly due to the removal of woody biomass but also, in the case of P, to reductions in soil pools. Mineral soil C, N, and P pools were 96%, 79%, and 69% of native soils, respectively. Although annual runoff from the watersheds was similar, the mined watershed exhibited taller, narrower storm peaks as a result of a higher soil bulk density and decreased infiltration rates. Stream export of N was much lower in the mined watershed due to lower net nitrification rates and nitrate concentrations in soil. However, stream export of sediment and P and summer stream temperature were much higher. Stream leaf decomposition was reduced and macroinvertebrate community structure was altered as a result of these changes to the stream environment. This land use change leads to substantial, long-term changes in ecosystem capital and function.