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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Autores principales: Zhi-Shan Zhang, Bing-Xin Xu, Yang Zhao, Ya-Fei Shi, Jian-Qiang Huo, Nan Wang
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Publicado: Elsevier 2021
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spelling oai:doaj.org-article:c2c331621dc5419c95e1d7c19492e5952021-12-01T05:00:48ZLong-term water balance variation after revegetation on the southeastern edge of the Tengger Desert1470-160X10.1016/j.ecolind.2021.108216https://doaj.org/article/c2c331621dc5419c95e1d7c19492e5952021-11-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S1470160X21008815https://doaj.org/toc/1470-160XMaintaining 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.Zhi-Shan ZhangBing-Xin XuYang ZhaoYa-Fei ShiJian-Qiang HuoNan WangElsevierarticleLysimeterRain-fedSand-binding shrubsScaling effectsSoil water availabilityEcologyQH540-549.5ENEcological Indicators, Vol 131, Iss , Pp 108216- (2021)
institution DOAJ
collection DOAJ
language EN
topic Lysimeter
Rain-fed
Sand-binding shrubs
Scaling effects
Soil water availability
Ecology
QH540-549.5
spellingShingle Lysimeter
Rain-fed
Sand-binding shrubs
Scaling effects
Soil water availability
Ecology
QH540-549.5
Zhi-Shan Zhang
Bing-Xin Xu
Yang Zhao
Ya-Fei Shi
Jian-Qiang Huo
Nan Wang
Long-term water balance variation after revegetation on the southeastern edge of the Tengger Desert
description 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.
format article
author Zhi-Shan Zhang
Bing-Xin Xu
Yang Zhao
Ya-Fei Shi
Jian-Qiang Huo
Nan Wang
author_facet Zhi-Shan Zhang
Bing-Xin Xu
Yang Zhao
Ya-Fei Shi
Jian-Qiang Huo
Nan Wang
author_sort Zhi-Shan Zhang
title Long-term water balance variation after revegetation on the southeastern edge of the Tengger Desert
title_short Long-term water balance variation after revegetation on the southeastern edge of the Tengger Desert
title_full Long-term water balance variation after revegetation on the southeastern edge of the Tengger Desert
title_fullStr Long-term water balance variation after revegetation on the southeastern edge of the Tengger Desert
title_full_unstemmed Long-term water balance variation after revegetation on the southeastern edge of the Tengger Desert
title_sort long-term water balance variation after revegetation on the southeastern edge of the tengger desert
publisher Elsevier
publishDate 2021
url https://doaj.org/article/c2c331621dc5419c95e1d7c19492e595
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AT yangzhao longtermwaterbalancevariationafterrevegetationonthesoutheasternedgeofthetenggerdesert
AT yafeishi longtermwaterbalancevariationafterrevegetationonthesoutheasternedgeofthetenggerdesert
AT jianqianghuo longtermwaterbalancevariationafterrevegetationonthesoutheasternedgeofthetenggerdesert
AT nanwang longtermwaterbalancevariationafterrevegetationonthesoutheasternedgeofthetenggerdesert
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