100-10 Experimental Evidence of Drought Induced Alternative Stable Soil Moisture States.

See more from this Division: SSSA Division: Soil Physics and Hydrology
See more from this Session: Symposium--Long-Term Terrestrial Observatories: Outdoor Laboratories for Soil-Plant-Atmosphere Interactions: I

Monday, November 16, 2015: 3:50 PM
Minneapolis Convention Center, 102 BC

David A. Robinson1, Scott B. Jones2, Inma Robinson3, Sabine Reinsch3, Maria T. DomĂ­nguez4, Andrew R. Smith5, Miles Marshall3 and Bridget A. Emmett3, (1)Deiniol Road, NERC-Centre for Ecology and Hydrology, Bangor, Gwynedd, UNITED KINGDOM
(2)Department of Plants, Soils and Climate, Utah State University, Logan, UT
(3)NERC-Centre for Ecology and Hydrology, Bangor, United Kingdom
(4)Instituto de Recursos Naturales y AgrobiologĂ­a de Sevilla, Sevilla, Spain
(5)Bangor University, Bangor, United Kingdom
Abstract:
The theory of alternative stable states in ecosystems is well established in ecology; however, evidence from manipulation experiments supporting the theory is limited. Developing the evidence base is important because it has profound implications for ecosystem management. Here we show evidence of the existence of alternative stable soil moisture states induced by drought in an upland wet heath. We used a long-term (15 yrs) climate change manipulation experiment with moderate sustained drought, which reduced the ability of the soil to retain soil moisture by degrading the soil structure, reducing moisture retention. Moreover, natural intense droughts superimposed themselves on the experiment, causing an unexpected additional alternative soil moisture state to develop, both for the drought manipulation and control plots; this impaired the soil from rewetting in winter. Our results show the coexistence of three stable states.

See more from this Division: SSSA Division: Soil Physics and Hydrology
See more from this Session: Symposium--Long-Term Terrestrial Observatories: Outdoor Laboratories for Soil-Plant-Atmosphere Interactions: I

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