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Table 1 (A) Pedoclimatic conditions: TAP, total annual precipitation; TSP, total summer precipitation (from May to August); MAT, mean annual temperature; MST, mean summer temperature; mean summer soil water content at 20 cm in depth in the different silvicultural systems, between 2009 and 2012. (B) Soil texture, composition, and pH for the 0–20- and 0–40-cm-deep layers at Guéméné-Penfao

From: Early effects of two planting densities on growth dynamics and water-use efficiency in Robinia pseudoacacia (L.) and Populus deltoides (Bartr. ex Marsh.) × P. nigra (L.) short rotation plantations

A

2009

2010

2011

2012

Climate

TAP (mm)

764

599

608

809

TSP (mm)

223

148

286

219

MAT (°C)

11.5

10.8

12.5

11.5

MST (°C)

16.7

16.7

16.2

16.4

Mean summer soil water content (%)

Black locust SRC

 

19.9 ± 2.1

17.6 ± 2.3

24.6 ± 1.9

Poplar SRC

 

17.5 ± 1.9

18.2 ± 3.1

26.8 ± 0.2

Black locust SRF

 

16.8 ± 1.9

14.8 ± 0.1

21.8 ± 0.9

Poplar SRF

 

14.1 ± 0.4

14.1 ± 0.2

21.3 ± 2.3

B

Soil layer

 

0–20 cm

 

20–40 cm

 

Texture (g kg−1)

Clay

200.0 ± 8.9

 

204.9 ± 7.3

 

Silt

212.9 ± 4.8

 

211.4 ± 5.3

 

Sand

187.1 ± 10.0

 

186.2 ± 9.3

 

Composition (g kg−1)

Organic C

23.0 ± 1.4

 

14.0 ± 0.8

 

Total N

1.7 ± 0.1

 

1.1 ± 0.1

 

Organic matter

39.8 ± 2.4

 

24.3 ± 1.4

 

pH

6.8 ± 0.1

 

6.6 ± 0.1