Relevant bibliographies by topics / Hyper-arid soil

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  1. Journal articles
  2. Dissertations / Theses

Academic literature on the topic 'Hyper-arid soil'

Author: Grafiati
Published: 4 June 2021
Last updated: 9 February 2022

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Journal articles on the topic "Hyper-arid soil"

1

Shao, Yaping, Klaus Fraedrich, and Masahide Ishizuka. "Modelling Soil Moisture in Hyper-Arid Conditions." Boundary-Layer Meteorology 179, no. 2 (2021): 169–86. http://dx.doi.org/10.1007/s10546-020-00596-9.

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AbstractIn most land-surface models, the evolution of soil moisture is governed by soil-hydraulic processes. In hyper-arid soils, these processes break down, but soil moisture continues to show clear temporal variations, suggesting that other processes may be at work. We hypothesize that moisture in such soils varies due to evaporation in the soil and to vapour fluxes at the air–soil interface. To test this, we include vapour exchange between the air and soil in a land-surface model, apply the model to a desert site, and compare the simulated and observed soil moisture. The good agreement betw
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Patzelt, Dominik J., Ladislav Hodač, Thomas Friedl, Nicole Pietrasiak, and Jeffrey R. Johansen. "Biodiversity of soil cyanobacteria in the hyper-arid Atacama Desert, Chile." Journal of Phycology 50, no. 4 (2014): 698–710. http://dx.doi.org/10.1111/jpy.12196.

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Lalley, Jennifer S., and Heather A. Viles. "Recovery of lichen-dominated soil crusts in a hyper-arid desert." Biodiversity and Conservation 17, no. 1 (2007): 1–20. http://dx.doi.org/10.1007/s10531-007-9153-y.

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Santhanam, Rakesh, Chinyere K. Okoro, Xiaoying Rong, et al. "Streptomyces deserti sp. nov., isolated from hyper-arid Atacama Desert soil." Antonie van Leeuwenhoek 101, no. 3 (2011): 575–81. http://dx.doi.org/10.1007/s10482-011-9672-0.

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Rahman, Shang, Shahid, and Wen. "Performance Assessment of SM2RAIN-CCI and SM2RAIN-ASCAT Precipitation Products over Pakistan." Remote Sensing 11, no. 17 (2019): 2040. http://dx.doi.org/10.3390/rs11172040.

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Accurate estimation of precipitation from satellite precipitation products (PPs) over the complex topography and diverse climate of Pakistan with limited rain gauges (RGs) is an arduous task. In the current study, we assessed the performance of two PPs estimated from soil moisture (SM) using the SM2RAIN algorithm, SM2RAIN-CCI and SM2RAIN-ASCAT, on the daily scale across Pakistan during the periods 2000–2015 and 2007–2015, respectively. Several statistical metrics, i.e., Bias, unbiased root mean square error (ubRMSE), Theil’s U, and the modified Kling–Gupta efficiency (KGE) score, and four cate
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Santhanam, Rakesh, Xiaoying Rong, Ying Huang, Barbara A. Andrews, Juan A. Asenjo, and Michael Goodfellow. "Streptomyces bullii sp. nov., isolated from a hyper-arid Atacama Desert soil." Antonie van Leeuwenhoek 103, no. 2 (2012): 367–73. http://dx.doi.org/10.1007/s10482-012-9816-x.

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7

Levi, Nathan, Noa Hillel, Eli Zaady, et al. "Soil quality index for assessing phosphate mining restoration in a hyper-arid environment." Ecological Indicators 125 (June 2021): 107571. http://dx.doi.org/10.1016/j.ecolind.2021.107571.

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Li, H., W. Wang, H. Zhan, F. Qiu, F. Wu, and G. Zhang. "The yearly amount and characteristics of deep-buried phreatic evaporation in hyper-arid areas." Hydrology and Earth System Sciences Discussions 12, no. 12 (2015): 13123–47. http://dx.doi.org/10.5194/hessd-12-13123-2015.

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Abstract. Water scarcity is the primary cause of land deterioration, so finding new available water resources is crucial to ecological restoration. We investigated a hyper-arid Gobi location in the Dunhuang Mogao Grottoes in this work wherein the burial depth of phreatic water is over 200 m. An air-conditioner was used in a closed greenhouse to condense and measure the yearly amount of phreatic evaporation (PE) from 2010 to 2015. The results show that the annual quantity of PE is 4.52 mm, and that the PE has sinusoidal characteristics. The average PE is 0.0183 mm d-1 from March to November. Ac
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Gordon, Gabrielle, Ilan Stavi, Uri Shavit, and Ravid Rosenzweig. "Oil spill effects on soil hydrophobicity and related properties in a hyper-arid region." Geoderma 312 (February 2018): 114–20. http://dx.doi.org/10.1016/j.geoderma.2017.10.008.

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LI, Zheng, Zeev RONEN, Faina GELMAN, Onn CROUVI, Gilboa ARYE, and Ravid ROSENZWEIG. "Reclamation of oil-induced soil hydrophobicity in the hyper-arid Evrona Nature Reserve, southern Israel." Pedosphere 31, no. 6 (2021): 892–902. http://dx.doi.org/10.1016/s1002-0160(21)60031-0.

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Dissertations / Theses on the topic "Hyper-arid soil"

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Prellwitz, Joel S. "A CHARACTERIZATION OF HYPER-ARID NITRATE SOILS IN THE BAQUEDANO VALLEY OF THE ATACAMA DESERT, NORTHERN CHILE." Miami University / OhioLINK, 2007. http://rave.ohiolink.edu/etdc/view?acc_num=miami1193748962.

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2

Lalley, Jennifer S. "Lichen-dominated soil crusts in the hyper-arid Namib Desert : anthropogenic impacts and conservation implications." Thesis, University of Oxford, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.417605.

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3

(9524549), Lucia De Lourdes Zuniga. "Transformation of the hyper-arid desert soils in Arequipa Peru during four decades of irrigated agriculture." Thesis, 2020.

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In Peru, nearly 32 million people rely heavily on human-made coastal irrigation agricultural hubs that rely on water from melting glaciers, snowpack, and rain transported by rivers and canals from high in the Andes. However, Peru’s water resources are in a vulnerable state as climate change has shifted rainfall patterns causing glacier retreat affecting nearly the loss of one-third of the glaciers. In recent decades, an increase and expansion of irrigation projects in Peru require agriculture practices to consider environmental impacts directly. Now is the time to explore the sustainability of
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