کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4573092 1332418 2016 10 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Soil-water repellency characteristic curves for soil profiles with organic carbon gradients
ترجمه فارسی عنوان
منحنی های ویژگی های خلل و فرج آبرفتی برای پروفیل های خاک با شیب های کربن آلی
کلمات کلیدی
ضد خش آب منحنی مشخصه خلال آب، آندوسول، پارامترهای ضد انعقاد کربن آلاینده خاک
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


• Water repellency at different soil organic carbon (SOC) contents was measured.
• Repellency was restricted to the top 20 cm of the soil profiles.
• The sessile drop method is highly sensitive at high SOC contents.
• We proposed six repellency parameters for repellent soils.
• Functions between those repellency parameters and the SOC content were fitted.

Soil water repellency (SWR) of soils is a property with significant consequences for agricultural water management, water infiltration, contaminant transport, and for soil erosion. It is caused by the presence of hydrophobic agents on mineral grain surfaces. Soils were samples in different depths at three forest sites in Japan and three pasture sites in New Zealand, covering soil organic carbon (SOC) contents between 1 and 26%. The SWR was measured over a range of water contents by three common methods; the water drop penetration time (WDPT) test, the molarity of an ethanol droplet (MED) method, and the sessile drop method (SDM). The aim to (i) compare the methods, (ii) characterize the soil-water repellency characteristic curves (SWRCC) being SWR as a function of the volumetric soil-water content (θ) or matric potential (ψ), and (iii) find relationships between SWRCC parameters and SOC content. The WDPT, MED, and SDM generally agreed well in predicting the θ range where SWR occurred, and there was close agreement between SWR results determined by average MED and SDM at similar θ. Generally, SWR was only found within the top 20 cm of the soil profiles. Six SWR parameters were introduced: (i) the area under the curve (SWR(θ)); (ii) θ at the maximum SWR (θWR-max), (iii) θ where SWR ceased (θnon-WR), (iv) the maximum SWR (CAi-max), (v) pF at the maximum SWR (pFWR-max) and (vi) pF where SWR ceased (pFnon-WR). The relationship between the first three parameters and SOC content were best described with Langmuir type equations (r2 of 0.5–0.7), while the other three parameters changed linearly with SOC contents.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Geoderma - Volume 264, Part A, 15 February 2016, Pages 150–159
نویسندگان
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