Zobrazeno 1 - 10
of 74
pro vyhledávání: '"William F. Bleam"'
The research was conducted in the Kırklareli stream, which flows southwest through the city of the same name toward the village of Kavaklı. The aim of the study is to evaluate water analysis results and assess the potential that the European Union
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ba88183a01e7afbcdca634592e64bcff
Autor:
Sultan Kıymaz, William F. Bleam
Seyfe Lake is an important part of the natural ecosystem of Central Anatolia and lies within a 1487 km2 closed basin. Groundwater withdrawal for irrigation and recent climatic change have caused lake area to decrease for decades and to completely dis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6cb900357ec3cb722d94e9d359ddff70
https://doi.org/10.20944/preprints202111.0180.v1
https://doi.org/10.20944/preprints202111.0180.v1
Publikováno v:
Geoderma. 353:449-458
Soil sodification and salinization present a global soil degradation risk to agricultural production since they affect soil hydraulic properties. Soils containing smectite clays have been found to be most sensitive to sodicity although little researc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d45775b8126657fb242c6ab8190d9cb
https://doi.org/10.1016/j.geoderma.2019.07.016
https://doi.org/10.1016/j.geoderma.2019.07.016
Publikováno v:
Geoderma. 376:114532
The use of low-quality water for irrigation is expected to keep increasing worldwide, which increases the risk of soil degradation. The response of soil to irrigation waters with excessive sodium depends on the soil clay behavior. Soil physical prope
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a1eebee8a4cdd9bddc21c8daabaf867
https://doi.org/10.1016/j.geoderma.2020.114532
https://doi.org/10.1016/j.geoderma.2020.114532
Autor:
William F. Bleam
Natural organic matter is a component of the terrestrial carbon cycle, representing both an important environmental substance and a vital component of the biological energy cycle. The reduced carbon in bioorganic compounds is kinetically stable in th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f9430b3433cf6f8a64d6b1d5eeff66c
https://doi.org/10.1016/b978-0-12-804178-9.00007-0
https://doi.org/10.1016/b978-0-12-804178-9.00007-0
Autor:
William F. Bleam
Environmental acidity and basicity arise from numerous sources: wash-out of atmospheric gases in the troposphere and their subsequent wet deposition on the land surface, fertilizer use and biomass harvest in agriculture, dissimilatory nitrate and sul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c4d596bbd96fc6994b28718ef782d8c5
https://doi.org/10.1016/b978-0-12-804178-9.00006-9
https://doi.org/10.1016/b978-0-12-804178-9.00006-9
Autor:
William F. Bleam
The clay minerals are of clay-grade phyllosilicates, phyllosilicate minerals whose natural occurrence is confined to the clay-size particle fraction. Clay minerals share another characteristic besides particle size: they form as low-temperature alter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bca763e6d47fe666860b6b675eb6c924
https://doi.org/10.1016/b978-0-12-804178-9.00003-3
https://doi.org/10.1016/b978-0-12-804178-9.00003-3
Autor:
William F. Bleam
Residence time, water-holding capacity, groundwater flow paths and rates, and transport models all contribute to our capacity to predict the impact of soil and aquifer properties on water chemistry and solute movement. A saturated zone water balance
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1550b4e2e2892682b9d765a3d4ddbc58
https://doi.org/10.1016/b978-0-12-804178-9.00002-1
https://doi.org/10.1016/b978-0-12-804178-9.00002-1
Autor:
William F. Bleam
Soil and environmental chemists simulate water chemistry using a host of chemical equilibrium reactions and constants. In most water chemistry problems we need to adjust concentrations using activity coefficients; otherwise the ion concentration prod
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::62025b400b97f833116bba0f9e54ca64
https://doi.org/10.1016/b978-0-12-804178-9.00005-7
https://doi.org/10.1016/b978-0-12-804178-9.00005-7