Arid
DOI10.1890/03-0567
Linkages between microbial and hydrologic processes in arid and semiarid watersheds
Belnap, J; Welter, JR; Grimm, NB; Barger, N; Ludwig, JA
通讯作者Belnap, J
来源期刊ECOLOGY
ISSN0012-9658
出版年2005
卷号86期号:2页码:298-307
英文摘要

Microbial activity in semiarid and and environments is closely related to the timing, intensity, and amount of precipitation. The characteristics of the soil surface, especially the influence of biological soil crusts, can determine the amount, location, and timing of water infiltration into desert soils, which, in turn, determines the type and size of microbial response. Nutrients resulting from this pulse then create a positive feedback as increases in microbial and plant biomass enhance future resource capture or, alternatively, may be lost to the atmosphere, deeper soils, or downslope patches. When rainfall intensity overwhelms the water infiltration capacity of the plant interspace or the plant patch, overland water flow links otherwise separated patches at many different scales via the transport of nutrients in water, soil, and organic matter. For example, material carried from the plant interspace is often deposited under an adjacent plant. Alternatively, material from both of these patches may be carried to rills that feed ephemeral channels, thence to seasonally intermittent and, finally, perennial streams. These inputs can either be retained by the stream-riparian ecosystem or be exported in surface flow. However, in larger perennial streams, the fate of these material inputs is confounded by the impact of storm-driven flows on the extant aquatic biota, as flash floods can also represent success ion-initiating disturbances to the stream-riparian ecosystem on a wide range of time scales. In contrast to uplands where precipitation initiates the microbial response, nutrient transfers can support a flush of plant uptake and microbial processing, triggered by high nutrient concentrations and changed nutrient form (e.g., nitrate or ammonium). The nature and strength of the linkages between the different ecosystem components define the structure and function of arid ecosystems. Losses of materials are natural processes, but it is problematic when conserving" systems become "leaky" via anthropogenic disturbance and losses exceed gains.


英文关键词activity pulse biological soil crusts desert infiltration nutrient cycling precipitation
类型Article
语种英语
国家USA ; Australia
收录类别SCI-E
WOS记录号WOS:000227634400004
WOS关键词SONORAN DESERT ECOSYSTEM ; SOIL CHEMICAL-PATTERNS ; SHORTGRASS STEPPE ; STREAM ECOSYSTEM ; NITROGEN ; BIOMASS ; GRASSLAND ; CRUSTS ; CARBON ; DENITRIFICATION
WOS类目Ecology
WOS研究方向Environmental Sciences & Ecology
来源机构United States Geological Survey ; Arizona State University ; Commonwealth Scientific and Industrial Research Organisation ; Colorado State University
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/148864
作者单位(1)US Geol Survey, Canyonlands Field Stn, SW Biol Sci Ctr, Moab, UT 84532 USA;(2)Arizona State Univ, Dept Biol, Tempe, AZ 85287 USA;(3)Colorado State Univ, Ft Collins, CO 80523 USA;(4)CSIRO Sustainable Ecosyst, Atherton, Qld 4833, Australia
推荐引用方式
GB/T 7714
Belnap, J,Welter, JR,Grimm, NB,et al. Linkages between microbial and hydrologic processes in arid and semiarid watersheds[J]. United States Geological Survey, Arizona State University, Commonwealth Scientific and Industrial Research Organisation, Colorado State University,2005,86(2):298-307.
APA Belnap, J,Welter, JR,Grimm, NB,Barger, N,&Ludwig, JA.(2005).Linkages between microbial and hydrologic processes in arid and semiarid watersheds.ECOLOGY,86(2),298-307.
MLA Belnap, J,et al."Linkages between microbial and hydrologic processes in arid and semiarid watersheds".ECOLOGY 86.2(2005):298-307.
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