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首页> 外文期刊>Animal Production Science >Estimating and mapping deep drainage risk at the district level in the lower Gwydir and Macquarie valleys, Australia
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Estimating and mapping deep drainage risk at the district level in the lower Gwydir and Macquarie valleys, Australia

机译:估算和绘制澳大利亚吉威迪尔和麦夸里河下游山谷地区的深层排水风险

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In the Murray–Darling Basin, irrigated agriculture, which produces rice, dairy, cotton and citrus, is a large consumer of water resources. Effective management of the water resource is therefore important to ensure sustainability of irrigated agriculture. In the lower Gwydir and Macquarie valleys, respectively located in northern and central New South Wales of Australia, extensive irrigated-cotton production is an important contributor to the nation’s export earnings. However, there are problems of excessive deep drainage (DD) in these regions. To address them requires soil and water quality information, but there is little quantitative information to plan for and implement improved water use efficiency. In this paper, we explore methods that could efficiently generate data on natural resources. First, we carried out an electromagnetic induction (EM38) survey to characterise broad soil profile types in the Ashley (lower Gwydir valley) and Trangie (lower Macquarie valley) districts. From the resulting apparent electrical conductivity (ECa, mS/m) data collected using an EM 38 (vertical mode of operation), soil profile sites were selected and sampled, followed by laboratory analysis carried to determine exchangeable cations and clay content. The soil data collected were analysed with a salt and leaching fraction (SaLF) model, based on specific water quality and quantity parameters, such as electrical conductivity of irrigation water (ECiw, dS/m) and rainfall (R, mm/year). Various water application rates (I) were also considered, to simulate irrigated cotton (I = 600 mm/year) and rice production (I = 1200 mm/year) as well as shallow water reservoirs (I = 1800 mm/year). For each irrigation scenario, DD values (mm/year) were estimated. An exponential function was used to describe the relationships between ECa values obtained with the EM38 and estimated DD. These relationships were then used to estimate DD at each of the EM38 survey sites, whereupon cut-off (zc) values were used for indicator transforms of the data. Using indicator kriging (IK) and various irrigation scenarios, we demonstrate the usefulness of this approach in identifying areas of high risk of DD exceeding various cut-off values (zc = 50, 75, 100 and 200 mm/year). Thus, we show where improvements in water-use efficiency could be achieved in the irrigated cotton growing districts of Ashley and Trangie.
机译:在默里-达令盆地,生产水稻,奶制品,棉花和柑橘的灌溉农业是水资源的大消耗国。因此,对水资源的有效管理对于确保灌溉农业的可持续性很重要。在分别位于澳大利亚新南威尔士州北部和中部的吉威迪尔和麦夸里河下游谷地,大量的灌溉棉花生产是该国出口收入的重要贡献。然而,在这些地区存在过度的深排水(DD)的问题。解决这些问题需要土壤和水质信息,但是很少有定量信息可用于计划和实施提高的用水效率。在本文中,我们探索了可以有效生成自然资源数据的方法。首先,我们进行了电磁感应(EM38)调查,以表征Ashley(格威迪尔河谷下游)和Trangie(麦格理河谷下游)地区广泛的土壤剖面类型。从使用EM 38(垂直操作模式)收集的表观电导率(ECa,mS / m)数据中,选择土壤剖面位置并进行采样,然后进行实验室分析以确定可交换的阳离子和粘土含量。根据特定的水质和水量参数,例如灌溉水的电导率(ECiw,dS / m)和降雨(R,mm / year),使用盐和浸出率(SaLF)模型对收集的土壤数据进行分析。还考虑了各种水施用量(I),以模拟灌溉棉花(I = 600毫米/年)和水稻产量(I = 1200毫米/年)以及浅水水库(I = 1800毫米/年)。对于每种灌溉方案,估计DD值(毫米/年)。指数函数用于描述通过EM38获得的ECa值与估计的DD之间的关系。然后将这些关系用于估计每个EM38调查站点的DD,然后将截止(zc)值用于数据的指标转换。使用指示器克里金法(IK)和各种灌溉方案,我们证明了该方法在确定DD的高风险区域超过各种临界值(zc = 50、75、100和200 mm /年)时的有用性。因此,我们展示了在Ashley和Trangie的棉花种植区可以提高用水效率。

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