Published September 1, 2022 | Version v1
Dataset Open

Biocrust impacts on dryland soil water balance: A path towards the whole picture

  • 1. China Agricultural University
  • 2. Northern Arizona University

Description

As a crucial living feature inhabiting the soil-atmosphere boundary, biocrusts play a vital role in liquid water or vapor transport through surface soil and thus have strong effects on soil water regimes. However, it remains unclear how biocrusts affect annual or multi-year soil water budgets through the regulation of evaporation outputs and NRW or infiltration inputs. Thus, we used automated microlysimeters to continually investigate the differences in evaporation and NRW rates between moss-dominated biocrusts and bare soil at 0−5 cm depth for two years. The upper 30 cm of soil moisture (θ) and water storage (W) of bare soil and biocrusts were also monitored. Our results showed that the daily evaporation rate (E) of biocrusts was 17% higher than bare soil. Especially after rainfall events, biocrusts had higher E and larger cumulative evaporation than bare soil. Besides, the daily NRW of biocrusts averaged 15% higher than bare soil over two years. Furthermore, biocrusts increased θ by 11%−76% at 0−10 cm depth but decreased θ by 32%−56% at 20−30 cm depth in comparison to bare soil, and they subsequently decreased W by 20% at 0−30 cm depth. Summarized annually, the NRW amount of biocrusts was 19% higher than bare soil, but at the same time the cumulative evaporation of biocrusts was also 19% higher than bare soil. Finally, biocrusts resulted in more water loss at shallow depth through evaporation and lessened total W throughout 0−30 cm depth of soil. These findings demonstrate that although biocrusts input more NRW into surface soil, these water inputs partially offset their intensified evaporation. Given that all rainfall water infiltrates into the soil in our study system, our findings indicate that biocrusts may have an overall negative effect on soil water balance there, while at the same time increasing water storage and availability of the deeper soil underlying biocrusts.

Notes

Funding provided by: National Natural Science Foundation of China
Crossref Funder Registry ID: http://dx.doi.org/10.13039/501100001809
Award Number: No. 42077010

Funding provided by: "Light of West China" Program of the Chinese Academy of Sciences*
Crossref Funder Registry ID:
Award Number: No. 2019

Funding provided by: Open Fund for Key Laboratory of Land Degradation and Ecological Restoration in Northwestern China of Ningxia University*
Crossref Funder Registry ID:
Award Number: No. LDER2022Z02

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