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Fragmentation of native vegetation was mainly regulated by soil drainage, as in poorly drained soils, crop production is almost unfeasible.
Vacant lots may provide ecosystem services such as stormwater runoff capture, but the extent of these functions will be regulated by soil hydrology.
The dynamics of this process is mainly regulated by soil physico-chemical properties (e.g., total metal content, humidity, clay and hydrous oxide content, organic matter, pH, redox conditions) [35].
Multiple regressions indicated that soil dry mass and NH4+-N shaped CH4 flux of grasslands, whereas CH4 flux of forest soils was regulated by soil pH and NO3−-N.
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Net N mineralization and nitrification were strongly regulated by land use, precipitation, soil water and temperature.
The instantaneous current under short circuit conditions was found to be less than 1 µA, depended weakly on soil water content and was most likely regulated by electrode-soil interfacial resistance.
The microbiological processes that are responsible for emissions of these GHGs (i.e., nitrification, denitrification, methanogenesis, and respiration) are regulated by interactions among soil redox potential, pH, carbon (C) content, temperature, water content, and oxidants, including oxygen (O2) and nitrate (NO3−) [4, 5, 6].
In addition, several studies have examined how the PP and defense related pathways are regulated by interactions between soil microorganisms and plant roots [ 15- 18].
As dunes develop across this cold desert chronosequence, microbial community composition was not regulated primarily by soil C, but by N and P availability and soil stresses in shrub soils, and exclusively by soil stresses in interspace soils.
These results suggest that the carbon transformation related to oxidative enzyme activity is regulated by the seasonal patterns of soil moisture, soil temperature, and the N concentration in desert soil.
During rainy seasons, however, hydrochemical changes in epikarst groundwater were regulated by both dilution and soil CO2 effects.
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