Long-term water balance variation after revegetation on the southeastern edge of the Tengger Desert

Maintaining the water balance of soil-vegetation systems is necessary for the ecological restoration of desertified regions. However, the major processes controlling water balance after revegetation remains unclear. To quantify the water balance after revegetation of moving sand dunes, we performed...

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Bibliographic Details
Main Authors: Huo, J.-Q (Author), Shi, Y.-F (Author), Wang, N. (Author), Xu, B.-X (Author), Zhang, Z.-S (Author), Zhao, Y. (Author)
Format: Article
Language:English
Published: Elsevier B.V. 2021
Subjects:
Online Access:View Fulltext in Publisher
LEADER 03359nam a2200625Ia 4500
001 10.1016-j.ecolind.2021.108216
008 220427s2021 CNT 000 0 und d
020 |a 1470160X (ISSN) 
245 1 0 |a Long-term water balance variation after revegetation on the southeastern edge of the Tengger Desert 
260 0 |b Elsevier B.V.  |c 2021 
856 |z View Fulltext in Publisher  |u https://doi.org/10.1016/j.ecolind.2021.108216 
520 3 |a Maintaining the water balance of soil-vegetation systems is necessary for the ecological restoration of desertified regions. However, the major processes controlling water balance after revegetation remains unclear. To quantify the water balance after revegetation of moving sand dunes, we performed an 18-year-long large-weighting lysimeter monitoring study in the Tengger Desert, northern China. We measured daily precipitation, evapotranspiration (ET), and drainage loss (DL) on an area revegetated with either Artemisia ordosica or Caragana korshinskii, two shrubs with different crown size and rooting depth, and with bare soil. Our results showed that the annual precipitation of 186 mm was partitioned to 64% evaporation and 23% DL on the bare soil control. However, the water balance changed after revegetation, with the vast majority of precipitation ending up as ET (93% in A. ordosica and 98% in C. korshinskii). The relationships of ET and DL with precipitation showed a quasi-steady state at annual scales, a varying state at seasonal scales, and a pulsed state at daily scales. We also observed spatiotemporal niche partitioning between the two shrubs, where differences in water use promoted their coexistence in the revegetated desert areas. Our study suggests that the density and area of revegetation should be controlled within a certain range in accordance with the underlying soil-vegetation water balance in desert regions. Otherwise, sand-binding revegetation would be degraded and the ecological benefits of dune fixation would be lost. © 2021 
650 0 4 |a Artemisia ordosica 
650 0 4 |a bare soil 
650 0 4 |a Bare soils 
650 0 4 |a Caragana korshinskii 
650 0 4 |a China 
650 0 4 |a Ecology 
650 0 4 |a evapotranspiration 
650 0 4 |a Evapotranspiration 
650 0 4 |a Landforms 
650 0 4 |a Long-term water balances 
650 0 4 |a Lysimeter 
650 0 4 |a Lysimeter 
650 0 4 |a Lysimeters 
650 0 4 |a niche partitioning 
650 0 4 |a precipitation (climatology) 
650 0 4 |a Rain-fed 
650 0 4 |a Rain-feed 
650 0 4 |a revegetation 
650 0 4 |a Revegetation 
650 0 4 |a rooting 
650 0 4 |a Sand-binding shrub 
650 0 4 |a Sand-binding shrubs 
650 0 4 |a Scaling effects 
650 0 4 |a Scaling effects 
650 0 4 |a Soil conservation 
650 0 4 |a Soil moisture 
650 0 4 |a Soil surveys 
650 0 4 |a Soil water availability 
650 0 4 |a Soil water availability 
650 0 4 |a Soil-vegetation 
650 0 4 |a soil-vegetation interaction 
650 0 4 |a Tengger Desert 
650 0 4 |a Vegetation 
650 0 4 |a Vegetation systems 
650 0 4 |a water budget 
650 0 4 |a Water supply 
700 1 |a Huo, J.-Q.  |e author 
700 1 |a Shi, Y.-F.  |e author 
700 1 |a Wang, N.  |e author 
700 1 |a Xu, B.-X.  |e author 
700 1 |a Zhang, Z.-S.  |e author 
700 1 |a Zhao, Y.  |e author 
773 |t Ecological Indicators