The variation in soil moisture and the appropriate groundwater table for desert riparian forest along the Lower Tarim River

2011 ◽  
Vol 21 (1) ◽  
pp. 150-162 ◽  
Author(s):  
Xiaodong Ma ◽  
Yaning Chen ◽  
Chenggang Zhu ◽  
Weihong Li
2013 ◽  
Vol 71 (10) ◽  
pp. 4579-4589 ◽  
Author(s):  
Guilin Liu ◽  
Alishir Kurban ◽  
Huanming Duan ◽  
Umut Halik ◽  
Abdimijit Ablekim ◽  
...  

2013 ◽  
Vol 71 (10) ◽  
pp. 4591-4591
Author(s):  
Guilin Liu ◽  
Alishir Kurban ◽  
Hanming Duan ◽  
Umut Halik ◽  
Abdimijit Ablekim ◽  
...  

2014 ◽  
Vol 11 (10) ◽  
pp. 14819-14856 ◽  
Author(s):  
Y. N. Chen ◽  
W. H. Li ◽  
H. H. Zhou ◽  
Y. P. Chen ◽  
X. M. Hao ◽  
...  

Abstract. Studies of the water use of the desert riparian forest plant community in arid regions and analyses of the response and adaptive strategies of plants to environmental stress are of great significance to the formulation of effective ecological conservation and restoration strategies. Taking two inland rivers in the arid regions of northwestern China, downstream of the Tarim River and Heihe River Basin as the research target regions, this paper explored the stem water potential, sap flow, root hydraulic lift, and characteristics of plant water sources of the major constructive species in the desert riparian forest, Populus euphratica and Tamarix ramosissima. Specifically, this was accomplished by combining the monitoring of field physiological and ecological indicators, and the analysis of laboratory tests. Then, the water use differences of species in different ecological environments and their ecological significance were analyzed. This study indicated that: (1) in terms of water sources, Populus euphratica and Tamarix ramosissima mainly used deep subsoil water and underground water, but the plant root system in the downstream of the Tarim River was more diversified than that in the downstream of the Heihe River in water absorption, (2) in terms of water distribution, Populus euphratica root possessed hydraulic lift capacity, but Populus euphratica root in the downstream of the Tarim River presented stronger hydraulic lift capacity and more significant ecological effect of water redistribution, (3) in terms of water transport, the plants in the downstream of the Heihe River can adapt to the environment through the current limiting of branch xylem, while plants in the downstream of the Tarim River substantially increased the survival probability of the whole plant by sacrificing weak branches and improving the water acquisition capacity of dominant branches; and (4) in terms of water dissipation, the water use and consumption of Populus euphratica at night exhibited no significant difference, but the water use and consumption of Populus euphratica in the downstream of the Tarim River in the day was significantly higher than that in the downstream of the Heihe River, and the essential reason for this is the groundwater depth. The ecology in the downstream of the Heihe River has been in balance in the maintenance and development stage, while desert riparian forest plants in the downstream of the Tarim River are still in severe arid stress.


2017 ◽  
Vol 37 (22) ◽  
Author(s):  
周洪华 ZHOU Honghua ◽  
李卫红 LI Weihong ◽  
李玉朋 LI Yupeng ◽  
王玉阳 WANG Yuyang ◽  
黄湘 HUANG Xiang

2013 ◽  
Vol 10 (5) ◽  
pp. 5643-5686
Author(s):  
A. Richard ◽  
S. Galle ◽  
M. Descloitres ◽  
J. M. Cohard ◽  
J. P. Vandervaere ◽  
...  

Abstract. Forests are thought to play an important role in the regional dynamics of the West African monsoon, through their capacity to extract water from permanent aquifers located deep in the soil and pump it into the atmosphere even during the dry season. This is especially true for riparian forests located at the bottom of the hillslopes. This coupling between the riparian forests and the permanent aquifers is investigated, looking for quantifying its contribution to the catchment water balance. To this end, use is made of the observations available from a comprehensively instrumented hillslope through the framework of the AMMA-CATCH (African Monsoon Multidisciplinary Analysis – Coupling the Tropical Atmosphere and the Hydrological Cycle) observing system. Attention is paid to measurements of actual evapotranspiration, soil moisture and deep groundwater level. A vertical 2-D approach is followed using the physically-based Hydrus 2-D model in order to simulate the hillslope hydrodynamics, the model being calibrated and evaluated through a multi-criteria approach. The model correctly simulates the hydrodynamics of the hillslope as far as soil moisture dynamics, deep groundwater fluctuation and actual evapotranspiration dynamics are concerned. In particular, the model is able to reproduce the observed hydraulic disconnection between the deep permanent groundwater table and the river. A virtual experiment shows that the riparian forest depletes the deep groundwater table level through transpiration occurring throughout the year so that the permanent aquifer and the river are not connected. Moreover the riparian forest and the deep groundwater table form a coupled transpiration system: the riparian forest transpiration is due to the water redistribution at the hillslope scale feeding the deep groundwater through lateral saturated flow. The annual cycle of the transpiration origin is also quantified. The riparian forest which covers only 5% of the hillslope generates 37% of the annual transpiration, this proportion reaching 57% during the dry season. In a region of intense anthropogenic pressure, forest clearing and its replacement by cropping could impact significantly the water balance at catchment scale with a possible feedback on the regional monsoon dynamics.


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