In the same sediments, δDwax values average −202±7‰ (1σ, n= 22) for the C28 n-alkanoic acid.
Whereas peak responses represent the threshold record of a sound or synthesis specification's highest values, average responses represent the most common characteristics.
The mean BD values (average of all soil layers and manure treatments) were 1.43, 1.37 and 1.26 Mg m−3 for NT, CP and MP, respectively.
The mean CI values (average of all soil layers and tillage systems) were 1.43, 1.22 and 1.06 MPa for M0, M30 and M60, respectively.
The precision (relative standard deviation better than 14%) and relative recovery values (average value of 106% for five independent samples) demonstrated the potential of the approach.
We find a wide variation of TiO2 abundances (from 0 to 10 wt%) for early mare volcanism (>2.6 Ga), whereas only medium to high TiO2 values (average = 6.8 wt%, minimum = 4.5 wt%) are found for younger mare units (<2.6 Ga).
The terra rossa δ13C values average − 20 ± 0.7‰ PDB and are interpreted to represent sediment deposited in a closed cave system under high summer temperatures and with well-drained soils.
A peak of high δ13CO2 values (average of −9.2‰) was observed on the day of PS application and was attributed to the dissociation of PS carbonates when mixed with the relatively acidic soil.
The output generated by such a procedure may turn on half-clever abstractions, in which complex circumstances resistant to direct measurement are reduced to more easily determined proxy values: average walking speed stands in for the "pace" of urban life, while the number of patent applications constitutes an index of "innovation", and so on.
Evaluate the difference in experimental and theoretical shear strength values: Average experimental shear strength = 200 kN.
Evaluate difference in experimental and theoretical shear strength values: Average experimental shear strength = 209.5 kN.
