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Relationship between sand dew and plant leaf dew and its significance in irrigation water supplementation in Guanzhong Basin, China

机译:关中盆地沙露与植物叶露的关系及其在灌溉补水中的意义

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摘要

Dew can serve as an important source of moisture for plants, biological crusts, insects and small animals in arid and semiarid basin. Dew amount and the relationship between sand dew and plant leaf dew were analyzed to understand dew transformation law under different condensation surfaces and its significance in irrigation water supplementation. During April 1-May 31, and September 1-October 31, 2018, field monitoring was carried out at the groundwater and environment site of Chang'an University, in Guanzhong Basin, China, using weighing method for sand dew measure, as well as leaf wetness sensors for plant leaf dew measure. Results showed that both sand dew and leaf dew manifested high frequency and low amount pattern. Their dew days (69days, 66days) accounted for 80% and 77% of rainless days (86days), but dew amount (6.56mm, 14.75mm) accounted for 3.3% and 7.4% of rainfall (198.2mm) in the same period, respectively. The average daily dew amount for sand was 0.054mm with a daily maximum of 0.22mm, and that for plant leaf was 0.12mm with a daily maximum of 0.78mm. Average daily leaf dew amount was about 2.2 times that of sand dew amount. Sand dew amount (W) was highly and positively correlated to leaf dew amount (D), and the fitting equation was W=0.237xD+0.044 (p0.01), which will provide a reference for the transformation between sand dew amount and leaf dew amount, and provide a theoretical basis for the evaluation of dew resources in a region. Moreover, dew harvesting is passive and mainly occurs in the natural states, which has no energy requirements, such as electrical energy. Dew harvesting system, as an independent system, can minimize the transportation cost of irrigation and entails low initial investment. And dew water quality is better once pretreated. Hence, artificial condensation surfaces and structure designed to maximize dew amount is of great significance in irrigation water supplementation.
机译:露水可以作为干旱和半干旱盆地中植物,生物结皮,昆虫和小动物的重要水分来源。分析了露水量以及沙水与植物叶水之间的关系,以了解不同凝结面下的露水转化规律及其在灌溉水补给中的意义。在2018年4月1日至5月31日以及9月1日至10月31日,在中国关中盆地长安大学的地下水和环境站点进行了现场监测,采用了称重法进行了沙露测量,并用于植物叶片露水测量的叶片湿度传感器。结果表明,沙露和叶露均表现出高频率和低模式。露水天数(69天,66天)分别占无雨天(86天)的80%和77%,而同期露水量(6.56mm,14.75mm)分别占降雨量(198.2mm)的3.3%和7.4%,分别。沙的平均日露量为0.054mm,日最大值为0.22mm,而植物叶片的日露量为0.12mm,日最大值为0.78mm。日平均叶露量约为沙露量的2.2倍。沙露量(W)与叶露量(D)高度相关且正相关,拟合方程为W = 0.237xD + 0.044(p <0.01),为沙露量与叶片之间的转化提供参考。露水量,为区域露水资源评价提供理论依据。而且,露水收获是被动的,并且主要发生在自然状态下,没有能量需求,例如电能。露水收集系统作为一个独立的系统,可以使灌溉的运输成本最小化,并且需要很少的初期投资。预处理后,露水的水质会更好。因此,为使露水量最大化而设计的人工凝结表面和结构在灌溉用水补充中具有重要意义。

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  • 来源
    《Environmental Geology》 |2019年第12期|354.1-354.10|共10页
  • 作者单位

    Changan Univ, Res Inst Water & Dev, 126 Yanta Rd, Xian 710054, Shaanxi, Peoples R China|Changan Univ, Sch Environm Sci & Engn, 126 Yanta Rd, Xian 710054, Shaanxi, Peoples R China|Changan Univ, Minist Educ, Key Lab Subsurface Hydrol & Ecol Effects Arid Reg, 126 Yanta Rd, Xian 710054, Shaanxi, Peoples R China;

    Changan Univ, Sch Environm Sci & Engn, 126 Yanta Rd, Xian 710054, Shaanxi, Peoples R China|Changan Univ, Minist Educ, Key Lab Subsurface Hydrol & Ecol Effects Arid Reg, 126 Yanta Rd, Xian 710054, Shaanxi, Peoples R China;

    Changan Univ, Sch Environm Sci & Engn, 126 Yanta Rd, Xian 710054, Shaanxi, Peoples R China;

    Changan Univ, Sch Environm Sci & Engn, 126 Yanta Rd, Xian 710054, Shaanxi, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Sand dew; Leaf dew; Correlation analysis; Dew harvesting; Irrigation water;

    机译:沙露;叶露;相关分析;露水收获;灌溉用水;

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