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The flow of carbon from plant roots through the microbial biomass is one of the key processes in terrestrial ecosystems. Roots release considerable amounts of organic materials which are utilized by microbes as substrate for biosynthesis and energy supply. The fate of photosynthates and other organic material in the soil-root environment under different conditions was studied using ¹⁴C-tracers. Soil structure and texture had a large effect on the turnover of the ¹⁴C-labelled materials through the microbial biomass. Finer, clayey soils tended to be more 'preservative' than coarser, sandy soils, i.e. larger amounts of ¹⁴C were incorporated in microbial biomass and soil organic matter fractions in clayey soils than in sandy soils. The soil nutrient status also appeared to affect organic matter turnover. At limiting plant-nutrient concentrations the utilization of ¹⁴C-labelled photosynthates seem to be hampered. Plant roots influenced the transformation of glucose and crop residues and the effect was attributed to plant-induced changes in mineral nutrient status. The mechanisms of this process and the consequences are discussed. A number of areas for future research are identified, including the potentials for manipulating rhizodeposition.

The detritus standing crop, microbial respiration, and macroinvertebrate biomass were examined in monthly samples from the riffle sections of a first-order woodland stream. Total detritus was remarkably constant; the average (with 95% CL) ash-free dry mass standing crop was 426.4 + 85.9 g/m^2 over the 14 mo of the study. Throughout the year benthic detritus was dominated by fine particulate detritus (<1 mm), which made up 68.9% of the total ash-free dry mass. Woody debris made up 8%, whole leaves 3.5%, and leaf fragments and other coarse particulate detritus accounted for 19.7% of the total standing crop. Decreases in standing crop were attributable to microbial respiration, macroinvertebrate assimilation, and downstream export. Microbial respiration annually removed 150% of the average standing crop, with the major effect on the smallest particle size category. Macroinvertebrate assimilation, defined as the sum of respiration and growth, removed 11.6% of the detritus standing crop annually. Shredders accounted for 20% of total animal assimilation, with the remaining 80% attributable to collectors and grazers. Based on monthly changes, it appears that total detritus standing crop is the result of the past discharge regime, which determines the overall amount of detritus present, and the rate of biological (microbial and invertebrate) processes, which determine the size and quality of the detritus particles. This suggests that detritus in streams, while strongly affected by both biotic and abiotic factors, may be in equilibrium within physical and biological constraints such that an annual steady-state system exists, similar to that for soil systems.

In an incubation study the effect of moisture content on CO₂-C production from manure at 25°C was determined. Different non-linear regression models were applied to describe cumulative CO₂-C evolution and a simple first-order model gave the best curve fit. Derived data from the curve fitting procedure were plotted against moisture content. A linear relationship between moisture content and microbial activity up to 50% of the water-holding capacity was followed by a curvilinear response between 50% of WHC and saturation. Equations describing the effect of moisture on dry matter decomposition are given.

Numerous potentially toxic compounds are entering Louisiana's inshore and nearshore coastal environments. To a large degree there is insufficient information for predicting the fate and effect of these materials in aquatic environments. Studies documenting the impact of petroleum hydrocarbons entering Louisiana coastal wetlands are summarized. Also included are research findings on factors affecting the persistence of petroleum hydrocarbons and other toxic organics (pentachlorophenol (PCP), 2,4-dichlorophenoxyacetic acid (2,4-D), creosote, etc.) in sediment-water systems. Sediment pH and redox conditions have been found to play an important role in the microbial degradation of toxic organics. Most of the hydrocarbons investigated degrade more rapidly under high redox (aerobic) conditions although there are exceptions (e. g., 1,1,1-trichloro-2,2-bis(4-chlorophenyl) (DDT) and polychlorobiphenyls (PCBs)). Some of these compounds, due to their slow degradation in anaerobic sediment, may persist in the system for decades.

The extent of 14C-imazaquin and 14C-imazethapyr abiotic vs. biotic degradation in soil was investigated. Degradation was measured in an in vitro system which allowed 90% recovery of applied herbicide. Triallate biodegradation is well documented and therefore used as a standard. Herbicide degradation was compared in two soils, a Cisne silt loam and a Drummer silty clay loam. Herbicide degradation in gamma-irradiated soil was compared to fresh soil. Biomass quantities were measured for the duration of the experiments. 14CO2 evolution, extractable parent, metabolites, and unextractable residue were measured. After 12 weeks of incubation, 95% of the radioactivity could be extracted as parent from sterilized soil. In unsterilized soil, imazaquin and imazethapyr degraded at a similar rate which was dependent upon soil type. All herbicides degraded slower in the Drummer soil and triallate degraded two to three times faster than the imidazolinones in either soil. 14C-imazaquin degradation products included 14CO2 and unextractable residues. The major product from 14C-imazethapyr degradation was 14CO2. Evolution of 14CO2 from an imazethapyr-treated Cisne soil, containing a serial dilution of activated charcoal, demonstrated that adsorption of herbicide was negatively correlated with degradation. Therefore imidazolinone microbial degradation is regulated by the amount of herbicide in soil solution as determined by soil characteristics.

The mineralization of 2,4-dinitrophenol (DNP) and changes in the DNP-mineralizing population over a wide range of DNP concentrations were monitored to evaluate the dynamics of the DNP-mineralizing populations in two soils (soils 1 and 2). Curves of CO2evolution were analyzed using nonlinear regression analysis and models incorporating parameters for population size and growth rate. The results of these analyses were compared to independent estimates of the DNP-mineralizing population from most-probable-number (MPN) determinations. The combined results of these analyses showed that 0.1 μg of DNP g-1of soil was too low a concentration to support maintenance or growth of the DNP-mineralizing population, whereas all higher concentrations supported either maintenance or growth of the population in soil 1. Independent estimates of population size showed good agreement between the nonlinear regression and MPN techniques, especially at initial DNP concentrations below 100 μg g-1. Estimates of both population size and maximum specific growth rate varied with concentration, possibly indicating the existence of two different DNP-mineralizing populations in soil 1. In the other soil tested (soil 2), the population of DNP-mineralizers was much lower than in the first soil, and no evidence of two populations was obtained. In soil 2, good agreement between the nonlinear regression and MPN estimates of population size was also obtained. Results of this study demonstrate the power of using testable models of population dynamics to obtain useful estimates of parameters of microbial growth and survival in soil.