Arid
SIMULATING DEEP PERCOLATION IN FLOOD-IRRIGATED MATURE PECAN ORCHARDS WITH RZWQM2
Deb, S. K.; Shukla, M. K.; Mexal, J. G.
通讯作者Deb, S. K.
来源期刊TRANSACTIONS OF THE ASABE
ISSN2151-0032
EISSN2151-0040
出版年2012
卷号55期号:6页码:2089-2100
英文摘要

The timing and amount of irrigation water are critical to the optimum production of pecans in semi-arid, irrigated agriculture systems. However, few tools are available to managers for measuring or estimating water use compared to deep percolation (DP) below the root zone. The RZWQM2 model was compared to the daily water balance method at two flood-irrigated mature pecan orchards, with different soil textures and depths to water table, in the lower Rio Grande Valley near Las Cruces, New Mexico, to characterize: (I) DP below the upper 100 cm soil profile, and (2) the effects of DP on water table levels. At site I (sandy loam) and site 2 (silty clay loam), comparisons between measured and simulated soil water contents at different soil depths during March to December in 2009 and 2010 demonstrated that RZWQM2 generally provided satisfactory predictions of soil water dynamics but consistently undepredicted soil water content after irrigation. Total estimated and simulated DP at site I were 489.1 and 445.2 mm in 2009, and 541.5 and 465.8 mm in 2010, respectively. Thus, at site 1, 25% to 29% of the applied water percolated below the root zone, but the model underpredicted these values by 3 to 4 percentage points. In contrast, total estimated DP at site 2 was 37% and 35% of the total water, and again the model underpredicted by 4 to 5 percentage points. Water table levels at site I were affected by DP following irrigation events. This was likely related to the relatively shallow water table and the highly permeable sandy loam soil in the upper layers. Nevertheless, the root zone water balance at site I did not appear to be influenced by the water table since downward hydraulic fluxes were predominant below 40 cm depth and soil water content remained constant at 160 cm depth. In contrast, the deeper water table at site 2 was not influenced by DP. Calibration and validation of RZWQM2 with field data at pecan orchards with different soil textures and water table depths allow managers to use the model to address water management issues to minimize DP while optimizing pecan production.


英文关键词Carya illinoinensis Deep percolation Groundwater table Root Zone Water Quality Model (RZWQM2) Soil texture Soil water content Water balance method
类型Article
语种英语
国家USA
收录类别SCI-E
WOS记录号WOS:000313998700007
WOS关键词WATER-QUALITY MODEL ; FIELD-MEASURED DATA ; ROOT-ZONE ; GROUNDWATER RECHARGE ; NITRATE MOVEMENT ; TILE DRAINAGE ; SOIL ; CROP ; BALANCE ; EVAPOTRANSPIRATION
WOS类目Agricultural Engineering
WOS研究方向Agriculture
来源机构New Mexico State University
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/175190
作者单位New Mexico State Univ, Dept Plant & Environm Sci, Las Cruces, NM 88003 USA
推荐引用方式
GB/T 7714
Deb, S. K.,Shukla, M. K.,Mexal, J. G.. SIMULATING DEEP PERCOLATION IN FLOOD-IRRIGATED MATURE PECAN ORCHARDS WITH RZWQM2[J]. New Mexico State University,2012,55(6):2089-2100.
APA Deb, S. K.,Shukla, M. K.,&Mexal, J. G..(2012).SIMULATING DEEP PERCOLATION IN FLOOD-IRRIGATED MATURE PECAN ORCHARDS WITH RZWQM2.TRANSACTIONS OF THE ASABE,55(6),2089-2100.
MLA Deb, S. K.,et al."SIMULATING DEEP PERCOLATION IN FLOOD-IRRIGATED MATURE PECAN ORCHARDS WITH RZWQM2".TRANSACTIONS OF THE ASABE 55.6(2012):2089-2100.
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