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Research Article

Comparing cork quality from Hafir-Zarieffet mountain forest (Tlemcen, Algeria) vs. Tagus basin Montado (Benavente, Portugal)

, ORCID Icon, & ORCID Icon | (Reviewing Editor)
Article: 1236431 | Received 19 May 2016, Accepted 09 Sep 2016, Published online: 17 Oct 2016

Figures & data

Figure 1. Climatic diagrams for the study areas, Hafir-Zarieffet (in black) and Benavente (in gray).

Notes: Data from the meteorological stations of Mefrouche (Hafir-Zarieffet, ZA) 34°51′ N, 1°16′ W (1961–1990 for the precipitation and 1975–1990 for temperature) and Salvaterra de Magos (Benavente, CL) 39°02′ N, 8°44′ W (1961–1990). Precipitation (in bars) and mean temperature (in lines).
Figure 1. Climatic diagrams for the study areas, Hafir-Zarieffet (in black) and Benavente (in gray).

Table 1. Pore variables measured in the transverse section of the cork samples at both regions

Table 2. Cork porosity of the transverse section of cork samples

Figure 2. Histogram for the pore area feature in all cork samples from Hafir-Zarieffet (ZA) and Benavente (CL).

Note: In bars is the frequency distribution of the number of pores and in lines is the curve for the cumulative percentage of pores.
Figure 2. Histogram for the pore area feature in all cork samples from Hafir-Zarieffet (ZA) and Benavente (CL).

Figure 3. Representation of pore centroids in a XY-scatter plot for all cork samplers at Hafir-Zarieffet (ZA) and Benavente (CL).

Note: Circle diameter is proportional to pore area located from cork back (minimum Y-value) to cork belly (maximum Y-value).
Figure 3. Representation of pore centroids in a XY-scatter plot for all cork samplers at Hafir-Zarieffet (ZA) and Benavente (CL).

Table 3. Eigenvalues, canonical correlation coefficients, and variance explained by the first two discriminant functions (F1 and F2)

Supplemental material

Supplementary_material.docx

Download MS Word (1.6 MB)