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Journal of Arid Land  2018, Vol. 10 Issue (6): 833-849    DOI: 10.1007/s40333-018-0027-9
Research article     
Sap flow characteristics and physiological adjustments of two dominant tree species in pure and mixed plantations in the semi-arid Loess Plateau of China
Yakun TANG1, Xu WU2,3, Yunming CHEN1,*()
1 State Key Laboratory of Soil Erosion and Dry-land Farming on the Loess Plateau, Northwest A&F University, Yangling712100, China;
2 State Key Laboratory of Soil Erosion and Dry-land Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and the Ministry of Water Resources, Yangling 712100, China
3 University of Chinese Academy of Sciences, Beijing 100049, China
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Abstract  

It is essential to understand the water consumption characteristics and physiological adjustments of tree species under drought conditions, as well as the effects of pure and mixed plantations on these characteristics in semi-arid regions. In this study, the normalized sap flow (SFn), leaf water potential, stomatal conductance (gs), and photosynthetic rate (Pr) were monitored for two dominant species, i.e., Pinus tabuliformis and Hippophae rhamnoides, in both pure and mixed plantations in a semi-arid region of Chinese Loess Plateau. A threshold-delay model showed that the lower rainfall thresholds (RL) for P. tabuliformis and H. rhamnoides in pure plantations were 9.6 and 11.0 mm, respectively, and the time lags (τ) after rainfall were 1.15 and 1.76 d for corresponding species, respectively. The results indicated that P. tabuliformis was more sensitive to rainfall pulse than H. rhamnoides. In addition, strong stomatal control allowed P. tabuliformis to experience low gs and Pr in response to drought, while maintaining a high midday leaf water potential (Ψm). However, H. rhamnoides maintained high gs and Pr at a low Ψm expense. Therefore, P. tabuliformis and H. rhamnoides can be considered as isohydric and anisohydric species, respectively. In mixed plantation, the values of RL for P. tabuliformis and H. rhamnoides were 6.5 and 8.9 mm, respectively; and the values of τ were 0.86 and 1.61 d for corresponding species, respectively, which implied that mixed afforestation enhanced the rainfall pulse sensitivity for both two species, especially for P. tabuliformis. In addition, mixed afforestation significantly reduced SFn, gs, and Pr for P. tabuliformis (P<0.05), while maintaining a high leaf water potential status. However, no significant effect of mixed afforestation of H. rhamnoides was observed at the expense of leaf water potential status in response to drought. Although inconsistent physiological responses were adopted by these species, the altered water consumption characteristics, especially for P. tabuliformis indicated that the mixed afforestation requires further investigation.



Key wordsnormalized sap flow      physiological adjustments      mixed afforestation      Pinus tabuliformis      Hippophae rhamnoides     
Received: 12 November 2017      Published: 07 November 2018
Corresponding Authors:
Cite this article:

Yakun TANG, Xu WU, Yunming CHEN. Sap flow characteristics and physiological adjustments of two dominant tree species in pure and mixed plantations in the semi-arid Loess Plateau of China. Journal of Arid Land, 2018, 10(6): 833-849.

URL:

http://jal.xjegi.com/10.1007/s40333-018-0027-9     OR     http://jal.xjegi.com/Y2018/V10/I6/833

[1] Bonal D, Guehl J M.2001. Contrasting patterns of leaf water potential and gas exchange responses to drought in seedlings of tropical rainforest species. Functional Ecology, 15(4): 490-496.
[2] Bucci S J, Scholz F G, Goldstein G, et al.2004. Processes preventing nocturnal equilibration between leaf and soil water potential in tropical savanna woody species. Tree physiology, 24(10): 1119-1127.
[3] Burgess S S O.2006. Measuring transpiration responses to summer precipitation in a Mediterranean climate: a simple screening tool for identifying plant water-use strategies. Physiologia Plantarum, 127(3): 404-412.
[4] Chen H S, Shao M G, Li Y Y.2008. Soil desiccation in the Loess Plateau of China. Geoderma, 143(1-2): 91-100.
[5] Chen Y P, Wang K B, Lin Y S, et al.2015. Balancing green and grain trade. Nature Geoscience, 8: 739-741.
[6] Clearwater M J, Meinzer F C, Andrade J L, et al.1999. Potential errors in measurement of nonuniform sap flow using heat dissipation probes. Tree Physiology, 19(10): 681-687.
[7] Du S, Wang Y L, Kume T, et al.2011. Sapflow characteristics and climatic responses in three forest species in the semiarid Loess Plateau region of China. Agricultural and Forest Meteorology, 151(1): 1-10.
[8] Fang S M, Zhao C Y, Jian S Q.2016. Canopy transpiration of Pinus tabulaeformis plantation forest in the Loess Plateau region of China. Environmental Earth Sciences, 75: 376.
[9] Franks P J, Drake P L, Froend R H.2007. Anisohydric but isohydrodynamic: seasonally constant plant water potential gradient explained by a stomatal control mechanism incorporating variable plant hydraulic conductance. Plant Cell & Environment, 30(1): 19-30.
[10] Gao X D, Li H C, Zhao X N, et al.2018. Identifying a suitable revegetation technique for soil restoration on water-limited and degraded land: Considering both deep soil moisture deficit and soil organic carbon sequestration. Geoderma, 319: 61-69.
[11] Granier A.1987. Evaluation of transpiration in a Douglas-fir stand by means of sap flow measurements. Tree Physioogy, 3(4): 309-320.
[12] Ivans S, Hipps L, Leffler A J, et al.2006. Response of water vapor and CO2 fluxes in semiarid lands to seasonal and intermittent precipitation pulses. Journal of Hydrometeorology, 7(5): 995-1010.
[13] Jian S Q, Zhao C Y, Fang S M, et al.2015. Evaluation of water use of Caragana korshinskii and Hippophae rhamnoides in the Chinese Loess Plateau. Canadian Journal of Forest Research, 45(1): 15-25.
[14] Jian S Q, Wu Z N, Hu C H, et al.2016. Sap flow in response to rainfall pulses for two shrub species in the semiarid Chinese Loess Plateau. Journal of Hydrology and Hydromechanics, 64(2): 121-132.
[15] Li G Q, Xu G H, Guo K, et al.2016. Geographical boundary and climatic analysis of Pinus tabulaeformis in China: Insights on its afforestation. Ecological Engineering, 86: 75-84.
[16] McDowell N, Pockman W T, Allen C D, et al.2008. Mechanisms of plant survival and mortality during drought: why do some plants survive while others succumb to drought? New Phytologist, 178(4): 719-739.
[17] Meinzer F C, Goldstein G, Franco A C, et al.1999. Atmospheric and hydraulic limitations on transpiration in Brazilian cerrado woody species. Functional Ecology, 13(2): 273-282.
[18] Meng Q H, Fu B J, Tang X P, et al.2008. Effects of land use on phosphorus loss in the hilly area of the Loess Plateau, China. Environmental Monitoring and Assessment, 139(1-3): 195-204.
[19] Ogle K, Reynolds J F.2004. Plant responses to precipitation in desert ecosystems: integrating functional types, pulses, thresholds, and delays. Oecologia, 141(2): 282-294.
[20] Priestley C H B, Taylor R J.1972. On the assessment of surface heat flux and evaporation using large-scale parameters. Monthly Weather Review, 100(2): 81-92.
[21] Reyes-Acosta J L, Lubczynski M W.2014. Optimization of dry-season sap flow measurements in an oak semi-arid open woodland in Spain. Ecohydrology, 7(2): 258-277.
[22] Reynolds J F, Kemp P R, Ogle K, et al.2004. Modifying the 'pulse-reserve' paradigm for deserts of North America: precipitation pulses, soil water, and plant responses. Oecologia, 141(2): 194-210.
[23] Schwinning S, Ehleringer J R.2001. Water use trade-offs and optimal adaptations to pulse-driven arid ecosystems. Journal of Ecology, 89(3): 464-480.
[24] Silvertown J, Araya Y, Gowing D.2015. Hydrological niches in terrestrial plant communities: a review. Journal of Ecology, 103(1): 93-108.
[25] Sperry J S, Hacke U G.2002. Desert shrub water relations with respect to soil characteristics and plant functional type. Functional Ecology, 16(3): 367-378.
[26] Steppe K, De Pauw D J W, Doody T M, et al. A comparison of sap flux density using thermal dissipation, heat pulse velocity and heat field deformation methods. Agricultural and Forest Meteorology, 150(7-8): 1046-1056.
[27] Swaffer B A, Holland K L, Doody T M, et al.2014. Water use strategies of two co-occurring tree species in a semi-arid karst environment. Hydrological processes, 28(4): 2003-2017.
[28] Tang Y K, Wen X F, Sun XM, et al.2014. The limiting effect of deep soilwater on evapotranspiration of a subtropical coniferous plantation subjected to seasonal drought. Advances in Atmospheric Sciences, 31(2): 385-395.
[29] Teklemariam T A, Lafleur P M, Moore T R, et al.2010. The direct and indirect effects of inter-annual meteorological variability on ecosystem carbon dioxide exchange at a temperate ombrotrophic bog. Agricultural and Forest Meteorology, 150(11): 1402-1411.
[30] Thomas F M, Foetzki A, Gries D, et al.2008. Regulation of the water status in three co-occurring phreatophytes at the southern fringe of the Taklamakan Desert. Journal of Plant Ecology, 1(4): 227-235.
[31] Trubat R, Cortina J, Vilagrosa A.2006. Plant morphology and root hydraulics are altered by nutrient deficiency in Pistacia lentiscus (L.). Trees, 20: 334-339.
[32] Wei Y F, Fang J, Liu S, et al.2013. Stable isotopic observation of water use sources of Pinus sylvestris var. mongolica in Horqin Sandy Land, China. Trees-Structure and Function, 27(5): 1249-1260.
[33] Wen J, Chen Y M., Tang Y K., et al.2017. Characteristics and affecting factors of sap flow density of Pinus tabuliformis and Hippophae rhamnoides in growing season in the hilly region of the Loess Plateau, China. Chinese Journal of Applied Ecology, 28(3): 763-771. (in Chinese)
[34] West A G, Hultine K R, Burtch K G, et al.2007. Seasonal variations in moisture use in a pi?on-juniper woodland. Oecologia, 153(4): 787-798.
[35] Wu J E, Liu W J, Chen C F.2017. How do plants share water sources in a rubber-tea agroforestry system during the pronounced dry season? Agriculture, Ecosystems & Environment, 236: 69-77.
[36] Xu B C, Li F M, Shan L.2010. Seasonal root biomass and distribution of switchgrass and milk vetch intercropping under 2:1 row replacement in a semiarid region in Northwest China. Communications in Soil Science and Plant Analysis, 41(16): 1959-1973.
[37] Xu H, Li Y.2006. Water-use strategy of three central Asian desert shrubs and their responses to rain pulse events. Plant and Soil, 285(1-2): 5-17.
[38] Xu H, Li Y, Xu GQ, et al.2007. Ecophysiological response and morphological adjustment of two Central Asian desert shrubs towards variation in summer precipitation. Plant Cell and Environment, 30(4): 399-409.
[39] Xu G Q, Li Y, Xu H.2011. Seasonal variation in plant hydraulic traits of two co-occurring desert shrubs, Tamarix ramosissima and Haloxylon ammodendron, with different rooting patterns. Ecological Research, 26(6): 1071-1080.
[40] Yang B, Wen X F, Sun X M.2015. Seasonal variations in depth of water uptake for a subtropical coniferous plantation subjected to drought in an East Asian monsoon region. Agricultural and Forest Meteorology, 201: 218-228.
[41] Zapater M, Bréda N, Bonal D, et al.2013. Differential response to soil drought among co-occurring broad-leaved tree species growing in a 15-to 25-year-old mixed stand. Annals of Forest Science, 70(1): 31-39.
[42] Zencich S J, Froend R H, Turner J V, et al.2002. Influence of groundwater depth on the seasonal sources of water accessed by Banksia tree species on a shallow, sandy coastal aquifer. Oecologia, 131(1): 8-19.
[43] Zeppel M, Macinnis-Ng C M O, Ford C R, et al.2008. The response of sap flow to pulses of rain in a temperate Australian woodland. Plant and Soil, 305(1-2): 121-130.
[44] Zha T S, Barr A G, van der Kamp G, et al.2010. Interannual variation of evapotranspiration from forest and grassland ecosystems in western canada in relation to drought. Agricultural and Forest Meteorology, 150(11): 1476-1484.
[45] Zhang H D, Wei W, Chen L D, et al.2017. Evaluating canopy transpiration and water use of two typical planted tree species in the dryland Loess Plateau of China. Ecohydrology. 10(4): e1830, doi: 10.1002/eco.1830.
[46] Zhao WZ, Liu B.2010. The response of sap flow in shrubs to rainfall pulses in the desert region of China. Agricultural and Forest Meteorology, 150(9): 1297-1306.
[47] Zhu L W, Zhao P, Wang Q, et al.2015. Stomatal and hydraulic conductance and water use in a eucalypt plantation in Guangxi, southern China. Agricultural and Forest Meteorology, 202: 61-68.
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