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Effects of Drip System Uniformity and Irrigation Amount on Water and Salt Distributions in Soil Under Arid Conditions

机译:干旱条件下滴灌系统均匀度和灌溉量对土壤水盐分布的影响

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摘要

The dynamics of water and salt in soil were monitored in the 2010 and 2011 growing seasons of cotton to evaluate the salinity risk of soil under drip irrigation in arid environments for different management practices of drip system uniformity and irrigation amount. In the experiments, three Christiansen uniformity coefficients (CU) of approximately 65, 80, and 95%(referred to as low, medium, and high uniformity, respectively) and three irrigation amounts of 50, 75, and 100%of full irrigation were used. The distribution of the soil water content and bulk electrical conductivity (ECb) was monitored continuously with approximately equally spaced frequency domain reflectometry (FDR) sensors located along a dripline. Gravimetric samples of soil were collected regularly to determine the distribution of soil salinity. A great fluctuation in CU of water content and ECb at 60 cm depth was observed for the low uniformity treatment during the irrigation season, while a relatively stable variation pattern was observed for the high uniformity treatment. The ECb CU was substantially lower than the water content CU and its value was greatly related to the water content CU and the initial ECb CU. The spatial variation of seasonal mean soil water content and seasonal mean soil bulk electrical conductivity showed a high dependence on the variation pattern of emitter discharge rate along a dripline for the low and medium uniformity treatments. A greater irrigation amount produced a significantly lower soil salinity at the end of the irrigation season, while the influence of the system uniformity on the soil salinity was insignificant at a probability level of 0.1. In arid regions, the determination of the target drip irrigation system uniformity should consider the potential salinity risk of soil caused by nonuniform water application as the influence of the system uniformity on the distribution of the soil salinity was progressively strengthened during the growing season of crop.
机译:在2010年和2011年的土壤中水和盐的动力学在2010年和2011年生长季节中监测,以评估干旱环境下滴灌的土壤的盐度风险,以实现滴水系统均匀性和灌溉量的不同管理措施。在实验中,三个基督徒均匀性系数(Cu)约为65,80和95%(分别称为低,培养基,高均匀性)和三种灌溉量为50,75和100%的全灌溉用过的。用沿着滴水粉的近似等间隔的频域反射测量(FDR)传感器连续地监测土壤含水量和散装电导率(ECB)的分布。定期收集土壤的重量样品以确定土壤盐度的分布。在灌溉季节期间,观察到在灌溉季节的低均匀性治疗中,观察到含水量和ECB在含水含量和ECB的巨大波动,同时对高均匀性处理观察到相对稳定的变化模式。 ECB Cu基本上低于水含量Cu,其值与水含量Cu和初始ECB Cu大大相关。季节性平均土壤含水量和季节性平均土着导电性的空间变化表现出沿着低均匀性处理的司机的发射极排放率的变化模式的高依赖性。更大的灌溉量在灌溉季节结束时产生了显着降低的土壤盐度,而系统均匀性对土壤盐度的影响在0.1的概率水平下是微不足道的。在干旱地区,目标滴灌系统均匀性的测定应考虑不均匀的水应用引起的土壤潜在的盐度风险,因为系统均匀性对土壤盐度分布的影响逐步加强作物季节。

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  • 来源
    《农业科学学报(英文版)》 |2013年第5期|924-939|共16页
  • 作者单位

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, P.R.China;

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, P.R.China;

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, P.R.China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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