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Journal of Arid Land
Journal of Arid Land  2023, Vol. 15 Issue (1): 63-76    DOI: 10.1007/s40333-023-0001-z     CSTR: 32276.14.s40333-023-0001-z
Research article     
Biocrust-induced partitioning of soil water between grass and shrub in a desert steppe of Northwest China
YANG Xinguo1,2,3,*(), WANG Entian1,2,3, QU Wenjie1,2,3, WANG Lei1,2,3
1Northwest National Key Laboratory Breeding Base for Land Degradation and Ecological Restoration, Ningxia University, Yinchuan 750021, China
2Key Laboratory of Restoration and Reconstruction of Degraded Ecosystems, Ministry of Education, Ningxia University, Yinchuan 750021, China
3Ecology and Environment College, Ningxia University, Yinchuan 750021, China
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Abstract  

Maintaining the stability of exotic sand-binding shrub has become a large challenge in arid and semi-arid grassland ecosystems in northern China. We investigated two kinds of shrublands with different BSCs (biological soil crusts) cover in desert steppe in Northwest China to characterize the water sources of shrub (Caragana intermedia Kuang et H. C. Fu) and grass (Artemisia scoparia Waldst. et Kit.) by stable 18O isotopic. Our results showed that both shrublands were subject to persistent soil water deficiency from 2012 to 2017, the minimum soil depth with CV (coefficient of variation) <15% and SWC (soil water content) <6% was 1.4 m in shrubland with open areas lacking obvious BSC cover, and 0.8 m in shrubland covered by mature BSCs. For C. intermedia, a considerable proportion of water sources pointed to the surface soil. Water from BSCs contributed to averages 22.9% and 17.6% of the total for C. intermedia and A. scoparia, respectively. C. intermedia might use more water from BSCs in rainy season than dry season, in contrast to A. scoparia. The relationship between shrub (or grass) and soil water by δ18O shown significant differences in months, which partly verified the potential trends and relations covered by the high variability of the water source at seasonal scale. More fine roots at 0-5 cm soil layer could be found in the surface soil layer covered by BSCs (8000 cm/m3) than without BSCs (3200 cm/m3), which ensured the possibility of using the surface soil water by C. intermedia. The result implies that even under serious soil water deficiency, C. intermedia can use the surface soil water, leading to the coexistence between C. intermedia and A. scoparia. Different with the result from BSCs in desert areas, the natural withdrawal of artificial C. intermedia from desert steppe will be a long-term process, and the highly competitive relationship between shrubs and grasses also determines that its habitat will be maintained in serious drought state for a long time.

Key words： desert steppe      biological soil crusts      water resource      Caragana intermedia      Artemisia scoparia     
Received: 13 October 2022      Published: 31 January 2023
Corresponding Authors: *YANG Xinguo (E-mail: xinguoyang1976@163.com)
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YANG Xinguo
WANG Entian
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WANG Lei
Cite this article:

YANG Xinguo, WANG Entian, QU Wenjie, WANG Lei. Biocrust-induced partitioning of soil water between grass and shrub in a desert steppe of Northwest China. Journal of Arid Land, 2023, 15(1): 63-76.

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http://jal.xjegi.com/10.1007/s40333-023-0001-z     OR     http://jal.xjegi.com/Y2023/V15/I1/63

Fig. 1 Location of the experimental site (a), landscape and habitat characteristics of the shrubland (b and c). (b), S-CK, shrubland without BSCs (biological soil crusts) cover; (c), S-BSC, shrubland with BSCs cover.
Fig. 2 Soil water contents in 0-300 cm (a-o) layer from 2012 to 2017. S-CK, shrubland with BSCs (biological soil crusts) cover; S-BSC, shrubland with BSCs cover; CK, natural grassland without replanted Caragana intermedia.
Fig. 3 Daily time series of relative increment in surface soil moisture (ISSM) in S-CK and S-BSC (biological soil crust) plots in the growth seasons (from May to October) during 2016-2017. (a), ISSM in S-CK and S-BSC; (b), SWC (soil water content) in 0-5 and 5-10 cm soil layers in S-CK; (c) SWC in 0-5 and 5-10 cm soil layers in S-BSC. S-CK, shrubland without BSCs cover; S-BSC, shrubland with BSCs cover.
Species Index Water source
Surface
(0-2 cm)		 Shallow
(2-30 cm)		 Middle
(30-70 cm)		 Deep
(>70 cm)
Caragana intermedia
(n=18)		 Average (%) 22.9 34.3 22.8 20.0
CV (%) 62.5 58.6 63.4 41.5
Range (%) 0.0-55.6 9.5-80.4 2.7-63.3 2.2-33.1
Artemisia scoparia
(n=12)		 Average (%) 17.9 41.6 22.1 18.0
CV (%) 81.3 73.9 108.2 67.1
Range (%) 3.7-47.2 8.3-90.7 1.2-76.1 3.0-36.0
Table 1 Average proportional water uptake from four potential soil sources for Caragana intermedia and Artemisia scoparia
Fig. 4 Water uptake percentage from different potential sources for Caragana intermedia and Artemisia scoparia in the rainy and dry seasons during 2016-2017. Water sources were defined as BSCs (biological soil crusts) ranging from surface (0-2 cm), shallow (2-30 cm), middle (30-70 cm) to deep (>70 cm). SWC, soil water content. Bars are standard errors.
Fig. 5 Fine root length density in 0-10 cm soil layer for Caragana intermedia in plots with (BSCs reserved) and without biological soil crusts (BSCs removed). Fine roots were defined as roots with a diameter within 0.5-2.0 mm. *, P<0.05 level. Bars are standard errors.
Plot Shrub morphological characters Biodiversity index
CA (m2) SH (m) BD (cm) CD (%) R H D E
S-CK 2.87±0.30 1.25±0.43 1.79±0.63 23.5±4.08 2.33±0.12 3.38±0.36 0.23±0.17 1.25±0.12
S-BSC 2.51±0.45 0.99±0.28 1.47±0.42 21.8±5.22 1.55±0.06 2.43±0.40 0.40±0.09 0.98±0.15
Table S1 Shrub morphological characters and biodiversity in S-CK and S-BSC
Plot Silt and clay (%) SOC (g/kg) TN (g/kg) TP (g/kg)
S-CK 11.08±5.08a 3.94±0.35a 0.29±0.07a 0.29±0.06a
S-BSC 15.44±7.04a 4.04±0.27a 0.23±0.06a 0.33±0.02a
Table S2 Information of surface soil (0-20 cm) in S-CK and S-BSC
Fig. S1 Upper-direct growth of roots in 0-20 cm soil layer for C. intermedia in the rainy season in 2018
Fig. S2 Soil water content and its CV (coefficient of variation) values in different soil layers during 2012-2017. CV-S1, CV values of soil water contents during 2012-2017 in S-CK plot; CV-S2, CV values of soil water contents during 2012-2017 in S-BSC plot; CV-CK, CV values of soil water contents during 2012-2017 in CK plot; AV-S1, average values of soil water contents during 2012-2017 in S-CK plot (shrubland without BSCs cover); AV-S2, average values of soil water contents during 2012-2017 in S-BSC plot (shrubland with BSCs cover); AV-CK, average values of soil water contents during 2012-2017 in CK plot (grassland without shrub).
Fig. S3 Root growth of A. scoparia from May to September
Fig. S4 Percentage of water uptake from four potential soil water sources for Caragana intermedia and Artemisia scoparia in the rainy and dry seasons during 2016-2017. Water sources were defined as BSCs (biological soil crusts) ranging from surface (0-2 cm), shallow (2-30 cm), middle (30-70 cm) to deep (>70 cm). Different uppercase letters indicate significant differences between C. intermedia and different water sources at P<0.05 level. Different lowercase letters indicate significant differences between A. scoparia and different water sources at P<0.05 level. * indicates significant differences between C. intermedia and A. scoparia at P<0.05 level. Bars are standard errors.
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