Wickramarachchi Kanchana, Betti Giacomo, Azam Gaus
Department of Primary Industries and Regional Development, Perth, WA 6000, Australia.
Grain Research and Development Corporation, Adelaide, SA 5065, Australia.
Plants (Basel). 2025 Mar 4;14(5):799. doi: 10.3390/plants14050799.
Strategic deep tillage (SDT) practices, such as soil mixing following the application of soil amendments, are promising approaches to alleviate topsoil water repellence and other subsoil constraints and improve crop productivity. However, there is a lack of knowledge on the effect of SDT on soil water dynamics, especially under water-limited environments. This study evaluates the effects of clay incorporation, soil inversion and deep soil mixing on soil water infiltration, surface evaporation rates, soil water storage and subsequent impacts on the below and aboveground growth of wheat ( L. var Scepter) in controlled environments. Results show that soil mixing significantly improved water infiltration compared to an untreated control. Clay incorporation exhibited the highest bare soil surface evaporation rates immediately and two years post-tillage, leading to substantial water losses under warm and dry ambient conditions. Despite improving soil water storage in deeper layers, high evaporation rates in clay-incorporated soils negatively impacted wheat growth, with reduced shoot biomass and root length density. Conversely, soil inversion and mixing-only treatments demonstrated balanced improvements in water infiltration, soil water use, and wheat shoot biomass. These findings underscore the trade-offs associated with SDT practices, particularly in managing soil water loss and crop productivity in water-limited environments. This study also highlights the need for the careful selection of SDT for soil amelioration strategies tailored to soil types and climatic conditions to enhance agricultural productivity and sustainability.
战略深耕(SDT)措施,如在施用土壤改良剂后进行土壤混合,是缓解表土斥水性和其他底土限制因素并提高作物生产力的有前景的方法。然而,关于战略深耕对土壤水分动态的影响,尤其是在水分受限环境下的影响,目前还缺乏相关知识。本研究在可控环境中评估了掺入黏土、土壤翻转和深层土壤混合对土壤水分入渗、地表蒸发速率、土壤储水量以及随后对小麦(L. var Scepter)地上和地下生长的影响。结果表明,与未处理的对照相比,土壤混合显著改善了水分入渗。掺入黏土在耕作后立即以及两年后表现出最高的裸土表面蒸发速率,在温暖干燥的环境条件下导致大量水分流失。尽管掺入黏土的土壤增加了深层土壤储水量,但高蒸发速率对小麦生长产生了负面影响,地上生物量和根长密度降低。相反,土壤翻转和仅混合处理在水分入渗、土壤水分利用和小麦地上生物量方面表现出平衡的改善。这些发现强调了与战略深耕措施相关的权衡,特别是在水分受限环境下管理土壤水分流失和作物生产力方面。本研究还强调,需要根据土壤类型和气候条件精心选择战略深耕措施,以制定土壤改良策略,提高农业生产力和可持续性。