Knowledge Resource Center for Ecological Environment in Arid Area
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
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ISSN | 2151-0032 |
EISSN | 2151-0040 |
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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