Soybeans (Glycine max. cv. Williams) were grown to maturity in soil columns within polyvinyl pipe and placed in greenhouses with charcoal filtered (CF) and nonfiltered (NF) air. In each greenhouse plants were grown with and without soil moisture stress (SMS). Targeted soil water potentials at 0.25 m for no SMS and between 0.45 and 0.60 m for the SMS regime were -0.05 and -0.45 M Pa, respectively. The 7 h (1000-1700 h EDT) mean O(3) concentrations (June-October) were 0.039 and 0.009 ppm in NF and CF air, respectively. Ozone and SMS in combination were less than additive in their effects on growth of the plant top and bean yields. Plants in CF air had 70% greater top weight, 58% more bean yield and 43% more root dry weight than in NF air. Both the plant and the seed weight from plants without SMS weighed 35% more than with SMS. Total root length in CF air for plants with and without SMS averaged 1.84 and 1.98 km, respectively, as compared to 1.59 and 1.66 km for plants with and without SMS in NF air. The resultsare different, so far as the combined effects of O(3) and SMS on yield and root growth are concerned, than in a similar field study by Heggestad and co-workers primarily because of the presence of a water table in the field but absence of it in the columns, as planned, in this experiment. It is unique to use large soil columns to study root distribution and length as related to the effects of ambient O(3) alone, and its combination with SMS.
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Sci Rep
January 2025
Department of Mining and Geological Engineering, University of Arizona, Tucson, AZ, 85721, USA.
The thermodynamic properties of frozen soil depend on its temperature state and ice content. Additionally, the permeability coefficient significantly affects both the temperature distribution and water movement. In this study, the dynamic variation of soil permeability coefficient with temperature is considered, the permeability coefficient is defined as a piecewise function with temperature as independent variable, and the hydrothermal coupling equation is established.
View Article and Find Full Text PDFJ Fluoresc
January 2025
College of Chemistry and Chemical Engineering, Shaoxing University, Shaoxing, 312000, P. R. China.
The fluorescence detection of amino compounds and the evaluation of their content in environmental samples are vital, not only for assessing food quality but also for studying soil organic matter. Here, we present the synthesis and application of a novel fluorescent probe, 4-(9-acridone)benzylmethyl carbonochloride (APE-Cl), for detecting amino compounds via a chloroformate reaction with fluorescence detection. The complete derivatization reaction of APE-Cl with amino compounds can be accomplished in aqueous acetonitrile within 5 min at room temperature, using 0.
View Article and Find Full Text PDFBiological soil crusts (or biocrust) are diminutive soil communities with ecological functions disproportionate to their size. These communities are composed of lichens, bryophytes, cyanobacteria, fungi, liverworts, and other microorganisms. Creating stabilizing matrices, these microorganisms interact with soil surface minerals thereby enhancing soil quality by redistributing nutrients and reducing erosion by containment of soil particles.
View Article and Find Full Text PDFJ Environ Manage
January 2025
State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, 210008, China. Electronic address:
In farmland shelterbelt systems, the decomposition and/or apoptosis of forest fine root litter could affect farmland soil properties at the tree-crop interface, particularly the soil nitrogen (N) cycling. However, how fine root litter affect the ammonia (NH) and nitrous oxide (NO) losses from farmland soil and the crop production is little known. A soil column experiment covering a whole rice season was conducted to evaluate the dynamics aforesaid in response to fine root litter of Populus (RP) and Metasequoia glyptostroboides (RM) with 0 and 240 kg ha N fertilizer input.
View Article and Find Full Text PDFSci Total Environ
January 2025
Temple University, Department of Civil and Environmental Engineering, 1947 North 12(th) Street, Philadelphia, PA 19122, United States. Electronic address:
The importance of pH in stormwater bioretention beds cannot be overstated since it impacts plant and microbial populations and removal of potentially toxic elements (PTEs) from stormwater runoff. This study investigated the effects of dolomite amendment on pH neutralization and subsequent PTE immobilization in bioretention media. To assess dolomite dissolution, pH neutralization, and PTE immobilization, engineered bioretention media was amended with different dolomite ratios and samples of dolomite-amended media were collected from two bioretention beds, one and two months after installation.
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