Stable annual pattern of water use by Acacia tortilis in Sahelian Africa.

Water use by mature trees of Acacia tortilis (Forsk.) Hayne ssp. raddiana (Savi) Brenan var. raddiana growing in the northern Sahel was continuously recorded over 4 years. Water use was estimated from xylem sap flow measured by transient heat dissipation. Concurrently, cambial growth, canopy phenology, leaf water potential, climatic conditions and soil water availability (SWA) were monitored. In addition to the variation attributable to interannual variation in rainfall, SWA was increased by irrigation during one wet season. The wet season lasted from July to September, and annual rainfall ranged between 146 and 367 mm. The annual amount and pattern of tree water use were stable from year-to-year despite interannual and seasonal variations in SWA in the upper soil layers. Acacia tortilis transpired readily throughout the year, except for one month during the dry season when defoliation was at a maximum. Maximum water use of about 23 l (dm sapwood area)(-2) day(-1) was recorded at the end of the wet season. While trees retained foliage in the dry season, the decline in water use was modest at around 30%. Variation in predawn leaf water potential indicated that the trees were subject to soil water constraint. The rapid depletion of water in the uppermost soil layers after the wet season implies that there was extensive use of water from deep soil layers. The deep soil profile revealed (1) the existence of living roots at 25 m and (2) that the availability of soil water was low (-1.6 MPa) down to the water table at a depth of 31 m. However, transpiration was recorded at a predawn leaf water potential of -2.0 MPa, indicating that the trees used water from both intermediary soil layers and the water table. During the full canopy stage, mean values of whole-tree hydraulic conductance were similar in the wet and dry seasons. We propose that the stability of water use at the seasonal and annual scales resulted from a combination of features, including an extensive rooting habit related to deep water availability and an effective regulation of canopy conductance. Despite a limited effect on tree water use, irrigation during the wet season sharply increased predawn leaf water potential and cambial growth of trunks and branches.

[1]  G. Goldstein,et al.  Atmospheric and hydraulic limitations on transpiration in Brazilian cerrado woody species , 1999 .

[2]  Maurizio Mencuccini,et al.  Climate influences the leaf area/sapwood area ratio in Scots pine. , 1995, Tree physiology.

[3]  Frederick C. Meinzer,et al.  Mechanisms contributing to seasonal homeostasis of minimum leaf water potential and predawn disequilibrium between soil and plant water potential in Neotropical savanna trees , 2005, Trees.

[4]  F. Do,et al.  Influence of natural temperature gradients on measurements of xylem sap flow with thermal dissipation probes. 2. Advantages and calibration of a noncontinuous heating system. , 2002, Tree physiology.

[5]  A. Granier,et al.  Reverse phenology and dry‐season water uptake by Faidherbia albida (Del.) A. Chev. in an agroforestry parkland of Sudanese west Africa , 1999 .

[6]  A. Berger,et al.  The water status of six woody species coexisting in the Sahel (Ferlo, Senegal) , 1996, Journal of Tropical Ecology.

[7]  A. Granier Une nouvelle méthode pour la mesure du flux de sève brute dans le tronc des arbres , 1985 .

[8]  K. G. McNaughton,et al.  Stomatal Control of Transpiration: Scaling Up from Leaf to Region , 1986 .

[9]  Derek Eamus,et al.  Ecophysiology of trees of seasonally dry tropics: Comparisons among phenologies , 2001 .

[10]  H. L. Penman Natural evaporation from open water, bare soil and grass , 1948, Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences.

[11]  W. Edmunds,et al.  Groundwater recharge estimation using chloride, stable isotopes and tritium profiles in the sands of northwestern Senegal , 1996 .

[12]  A. P. O'Grady,et al.  Transpiration increases during the dry season: patterns of tree water use in eucalypt open-forests of northern Australia. , 1999, Tree physiology.

[13]  D. L. Scarnecchia,et al.  The Grazing Land Ecosystems of the African Sahel , 1991 .

[14]  P. Cook,et al.  Water balance of a tropical woodland ecosystem, Northern Australia: a combination of micro-meteorological, soil physical and groundwater chemical approaches , 1998 .

[15]  L. Hutley,et al.  Dry season conditions determine wet season water use in the wet-tropical savannas of northern Australia. , 2000, Tree physiology.

[16]  B. Köstner,et al.  Sapflow measurements in forest stands: methods and uncertainties , 1998 .

[17]  Dr. Henk Breman,et al.  Woody Plants in Agro-Ecosystems of Semi-Arid Regions , 2011, Advanced Series in Agricultural Sciences.

[18]  Derek Eamus,et al.  Seasonal Patterns in Soil Moisture, Vapour Pressure Deficit, Tree Canopy Cover and Pre-dawn Water Potential in a Northern Australian Savanna , 1997 .

[19]  S. Allen,et al.  Measurements of transpiration from savannah shrubs using sap flow gauges , 1995 .

[20]  Olivier Gimenez,et al.  Environmental influence on canopy phenology in the dry tropics , 2005 .

[21]  É. L. Floc’h,et al.  Acacia raddiana, un arbre des zones arides à usages multiples , 2003 .

[22]  L. Urban,et al.  Granier's Thermal Dissipation Probre (TDP) method for measuring sap flow in trees : theory and practice , 2004 .

[23]  Stan D. Wullschleger,et al.  A review of whole-plant water use studies in tree. , 1998, Tree physiology.

[24]  W. Edmunds,et al.  Nitrogen in interstitial waters in the Sahel; Natural Baseline, Pollutant or Resource? , 2005, Plant and Soil.