Soil structure, which refers to aggregates and pore characteristics, reflects the spatial arrangement of soil particles is a key component for crop yield health. Well-formed structure has favorable size distribution, supports water flow retention healthy plant growth. Compost biochar, important organic amendments, have potential influence but their effects on specific types properties not been ...

A few studies on outdoor human thermal comfort (HTC) have been conducted in the tropical region a hot and humid climate; however, there is paucity of discussions how exactly different spatial settings influence HTC. Thus, this paper aims to examine land use cover (LULC) affects HTC basis simulation Predicted Mean Vote (PMV) Physiologically Equivalent Temperature (PET) indices via ENVI-met Rayma...

Acute and chronic ecotoxicity tests with zinc were performed with the earthworm Eisenia fetida, the potworm Enchytraeus albidus, and the springtail Folsomia candida. To assess the influence of the soil type on zinc toxicity for these soil invertebrates, these tests were carried out in a standard artificial soil, a sandy and a loamy field soil. Based on the results of this experimental work and ...

We present a field application of a new in situ technique to analyze phase transformations of fine lead oxide particles (50-100mum) in different soils directly in the field over 18 months. After the first month of exposure to a calcareous sand we found newly precipitated secondary mineral phases on the lead oxide. The samples exposed to two loamy soils (Dystric Cambisol and Luvisol) showed only...

Nematodes of three genera (Acrobeloides sp., Aphelenchus avenae, and Scutellonema brachyurum) were induced to coil and enter anhydrobiosis in drying soil of two types: sandy loam and loamy sand. Coiling was studied in relationship to soil moisture characteristics. Coiling and the physiological state of anhydrobiosis occurred before the water in sandy soils reached a water potential of -15 bars....

Recently, Hilhorst (2000) presented a theoretical model describing a linear relationship between bulk electrical conductivity, o0, and dielectric constant, K„, in moist soil. Hilhorst (2000) found that using this linear relationship, measurements of the pore water electrical conductivity, ap, can be made in a wide range of soil types without soil-specific calibrations. If accurate measurements ...