4.7 Article

Tillage timing to improve soil water storage in Mediterranean long fallow

期刊

AGRICULTURAL WATER MANAGEMENT
卷 272, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.agwat.2022.107835

关键词

Dryland wheat; Evaporation; Water infiltration; Soil mulch; Notill; Seed-zone

资金

  1. USDA-Agricultural Research Service
  2. Washington State University Agricultural Research Center through Hatch Project [1017286]

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The study aimed to investigate the effect of delaying the creation of dry soil mulch at different times in late spring and summer on weed-free fallow for winter wheat in drylands. Results showed that seed-zone water and total stored water produced by different tillage timings remained surprisingly constant.
Creation of a dry soil mulch to maintain near-surface moisture in dry environments is an ancient practice that is still used in many regions of the world for timely establishment of crops after long fallow. Before availability of herbicides, the first tillage during fallow was timed to kill weeds, but now the optimum timing for tillage depends only on the interplay of evaporation and infiltration of rain. The goal is to maximize total root zone water storage and seed-zone water at seeding time. Our objective was to measure the effect of delaying soil mulch creation progressively later in the spring and summer on weed-free fallow for winter wheat (Triticum aestivum L.) in the Mediterranean inland Pacific Northwest drylands of the United States. Over a period of six years and a total of 12 site-years, four to seven tillage timings were compared to an untilled treatment. Soil water was measured at seeding time in the seed zone and total root zone. Seed-zone water and total stored water produced by different tillage timings was surprisingly constant, with few statistically significant or substantial differences. On average, only 2% of stored water was lost in the top 1.0 m of soil over 80 days during the hot, dry period towards the end of fallow. Responses to late spring rain could be seen, and tillage near the end of June (early summer) often produced maximum soil water content.

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