Sentence examples for soils and maximum from inspiring English sources

Hyperexponential retention profiles (RPs) were observed in both soils and maximum concentrations of 100 130 mg kg−1 were determined near the columns' inlet.

Delineating site-specific management zones is increasingly attracting attentions due to the need in understanding the intrinsic relationship between spatially varied productivity and soil characteristics, and growing public concern about the productivity of soils and maximum efficiency of crop inputs.

By studying the soil moisture characteristic curve at the difference treatment levels (0.12, 0.24, 0.36 and 0.48 g of crumb rubber/kg soil), it was revealed that by addition of CR application rate, water content increased at each suction point in both types of soils and maximum water content was gained at highest application rate of CR (0.48 g kg−1) (Fig. 1).

The minimum height was observed in control (soil) and maximum was observed in T4 (at the end of the experiment).

In addition, we propose a modification of the Choudhury et al. (1994) approach based on field-based experimental evidence of a minimum Kcb greater than 0. For sites with limited field data, we also analyze the utility of a simple linear regression based on the Kcb and SAVI values for bare soil and maximum Kcb values.

However, minimum soil disturbance and maximum soil cover are key elements of no-till for saving water and improving yields.

The differences found with respect to the native forest appear to indicate that the afforested soils have not yet reached their maximum soil quality and maximum potential as soil organic carbon sink.

International studies of poplar and willow plants established from cuttings to assess biomass for fuel potential indicate heights and aerial cover values similar to naturally established trees if the soil profile contains intermediate levels of fine textured soils and the maximum depth to groundwater is within 1.5 m of the ground surface (Caplan et al. [2012]).

REW is defined as the ratio between available soil water and maximum extractable water (i.e., water holding capacity) and varies between 1 (field capacity) and 0 (permanent wilting point).

None of the posterior distributions for the constant or size parameters (αj, β1j and β2j in Eqn (4)) included 0, while the least significant deviations from zero were seen for soil type and maximum wind speed parameters, and for the species Liquidambar styraciflua, Thuja occidentalis and Nyssa slyvatica.

The model used several interesting temperature adjustments to account for the differences between air temperature and soil minimum and maximum and canopy temperatures.