SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 1 May 2008
Published in Soil Sci Soc Am J 72:808-814 (2008)
DOI: 10.2136/sssaj2007.0074
© 2008 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Google Scholar
Right arrow Articles by Wu, L.
Right arrow Articles by Enloe, H. A.
PubMed
Right arrow Articles by Wu, L.
Right arrow Articles by Enloe, H. A.
Agricola
Right arrow Articles by Wu, L.
Right arrow Articles by Enloe, H. A.
Related Collections
Right arrow Water Management
Right arrow Carbon Sequestration

SOIL & WATER MANAGEMENT & CONSERVATION

Carbon Sequestration and Dynamics of Two Irrigated Agricultural Soils in California

Laosheng Wua,*, Yvonne Wooda, Pingping Jianga, Lianqin Lib, Genxing Panb, Jianhang Lua, Andrew C. Changa and Heather A. Enloec

a Dep. of Environmental Science, Univ. of California, Riverside, CA 92521
b Inst. of Resour., Ecosyst. and Environ. of Agric., Nanjing Agricultural Univ., Nanjing 210095, PRC
c Dep. of Renewable Resources, Univ. of Wyoming, Laramie, WY 82071

* Corresponding author (Laowu{at}mail.ucr.edu).

Irrigation in semiarid regions can alter soil C sequestration processes compared with those of native soils. To better understand the effect of these altered processes, we studied the C sequestration and dynamics of two soils from major irrigated agricultural regions of California (the San Joaquin Valley and the Imperial Valley). Soils were sampled from selected native and cultivated fields to represent a span of almost a century of irrigated farming. Field soil samples were analyzed for total soil C and soil inorganic C as carbonate (SIC). Soil organic C (SOC) was then calculated from the measured data. Results showed that SOC stock increased above that stored in the native soil after five decades of irrigated farming. The SIC stock showed opposing trends within the top meter of the two studied soils: a decrease was measured after 55 yr in the San Joaquin Valley soil, while SIC in the Imperial Valley soil increased after 85 yr of irrigated agriculture and appears to represent a significant form of sequestered soil C. Our results indicate that long-term irrigated farming can significantly increase SOC due primarily to SOC added below the 10-cm soil depth, while significant increases in SIC may be partially due to the conversion of increased soil CO2 to carbonates under a regime of Colorado River irrigation water. Thus, when considering C sequestration in irrigated agriculture in semiarid regions, it is important to determine levels of both SOC and SIC.

Abbreviations: MP, Imperial Valley • OM, organic matter • SIC, soil inorganic carbon • SJV, San Joaquin Valley • SOC, soil organic carbon • SOM, soil organic matter







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 2008 by the Soil Science Society of America.