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Analysing the Benefits of Growing Crops after Rice in the Rice Growing Areas in Australia

机译:在澳大利亚水稻种植区分析水稻种植后农作物的效益

摘要

The Murrumbidgee Irrigation Area (MIA), the Coleambally Irrigation Area (CIA), and theudMurray Valley (MV) constitute the major Australian rice growing areas and are located inudsouthern east Australia. According to the Ricegrowers' Association of Australia Inc. (2002),udthe annual value of production of rice was $357 million in 2001 and the industry generatesudmore than $500 million from value-added exports annually, allowing these rice growing areasudto play a significant role in the Australian economy.udThe rice growing areas are also among the areas where the sustainability of irrigatedudagriculture is under threat from rising watertables, soil salinity and other environmentaludconsequences. The depth to watertables in more than 70 per cent of the MIA (MIAudL&WMP, 1998), around 35 per cent of the CIA (CICL, 2001), and around 60 per cent of theudMV (Murray Irrigation, 2001) is now around two metres from the soil surface. With theudcurrent land use practices, around 20 to 30 per cent of regions such as the MIA couldudbecome moderately salinised in the next 30 years due to rising watertables (Humphreys et al.,ud2001). Water leaching and run-off from rice-based farms form further problems.udPaddocks are flood-irrigated during rice growing period between November to March.udAlthough irrigation water is released prior to rice harvest, much of the water is retained byudthe soil even after rice harvest. The soil then slowly drains this water along with the addedudwinter rainwater into the watertable beyond the root zone. This wet soil profile has theudpotential to become an extra economic resource for rice-based farms whenever it can be usedudto grow another crop during winter straight after rice.udGrowing winter crops immediately after rice harvest may reduce the amount of wateruddrainage into watertables on rice-based farms. Successful adoption of this potentiallyudattractive option seems to depend on good weather and rootzone water conditions, gooduddrainage and timeliness in the rice harvesting, stubble burning, and winter crop sowingudoperations. Among the constraints for adding crops after rice are too much rain orudwaterlogging for the winter crop to survive, problems with stubble burn, pests, weeds, andudunsuitable machinery leading to a high risk of crop failure (Humphreys and Bhuiyan, 2001).udAs one of the strategies to overcome the problems of rising watertables in rice growing areas,udthe Rice CRC is conducting Project 1205 “Quantifying and Maximising the Benefits of Cropsudafter Rice”, henceforward referred to as Project 1205. Project 1205 aims at determining theudconstraints and the success factors for rice growers to produce winter crops and pasturesudafter rice, and at measuring the impacts of this practice on environmental and economicudsustainability. In particular, the project aims to measure the effects of growing wheat afterudrice on the productivity and water use efficiency of the rice-wheat cropping system.ud2udThe objectives of this economic analysis of project 1205 are:ud· To identify the common crop rotations in the main Australian rice-based farming systems,udboth with and without crops after rice;ud· To estimate the potential financial benefits of growing crops after rice;ud· To identify the economic benefits to the community from reduced accessions toudgroundwater; andud· To compare returns with the costs to the CRC and its partners of developing andudextending this technology.udTo measure the likely financial and economic benefits of growing crops after rice, the studyudrelied heavily on the results from Humphreys et al. (2001).
机译:Murrumbidgee灌溉区(MIA),Coleambally灌溉区(CIA)和 udMurray谷(MV)构成澳大利亚主要的水稻种植区,位于澳大利亚东部南部。根据澳大利亚稻米种植者协会(2002)的统计,2001年稻米的年产值为3.57亿澳元,该行业每年从增值出口中产生的乌迪尼加5亿澳元,这使这些稻米种植区在澳大利亚经济中发挥着重要作用。 ud水稻种植地区也是受地下水位上升,土壤盐碱化和其他环境 u后果影响的灌溉 udagridculture的可持续性的地区之一。超过70%的MIA(MIA udL&WMP,1998),大约35%的CIA(CICL,2001)和大约60%的 udMV(Murray Irrigation,2001)的地下水位现在距土壤表面约两米。在目前的土地使用方式下,由于地下水位的上升,未来30年中,诸如MIA等地区的约20%至30%的盐渍化程度将逐渐提高(Humphreys等, ud2001)。稻田农场的水流失和径流形成了进一步的问题。 ud在11月至3月的水稻生长期间,对小牧场进行了洪水灌溉。 ud尽管灌溉水是在水稻收割之前释放的,但大部分水分仍被 udthe保留。即使收割水稻也能保持土壤。然后,土壤将这种水和添加的/冬雨水慢慢地排到根部区域以外的地下水位中。这种湿润的土壤剖面有潜力在任何时候都可以用作水稻农场的额外经济资源在稻米过后的整个冬季直接种植另一种作物。 ud稻米收获后立即种植冬季作物可能会减少水量在稻田中将水排入地下水。成功采用这种潜在的/缺乏吸引力的选择似乎取决于良好的天气和根区水条件,水稻收割,秸秆焚烧和冬季作物播种/作业的良好/排水和及时性。稻米增产的制约因素包括:雨水过多或积水过多,冬季农作物无法生存;发茬烧伤,病虫害,杂草和不适当的机械问题导致农作物歉收的风险很高(Humphreys and Bhuiyan,2001)。作为克服水稻种植区地下水位上升问题的策略之一, udice CRC正在实施项目1205“量化和最大化农作物的收益”,因此被称为项目1205。项目1205的目标在确定水稻种植者生产冬季作物和草场后的水稻的约束和成功因素,并衡量该做法对环境和经济可持续性的影响。特别是,该项目旨在衡量“干旱后种植小麦”对稻麦种植系统的生产力和水分利用效率的影响。 ud2 ud项目1205的经济分析的目标是: ud·澳大利亚主要稻米种植系统中常见的农作物轮换, ud大米后有或没有农作物; ud·估计大米后种庄稼的潜在经济利益; ud·从中确定对社区的经济利益减少对地下水的加入;和 ud·为了将收益与CRC及其合作伙伴开发和扩展该技术的成本进行比较。 ud为了衡量水稻种植后种植农作物可能带来的经济和经济利益,该研究在很大程度上依赖于Humphreys等人的结果。等(2001)。

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