کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6413821 1629964 2013 10 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Specific processes during in situ infiltration into a sandy soil with low-level water repellency
ترجمه فارسی عنوان
فرآیندهای خاص در طی نفوذ در محل به خاک ماسه ای با دفع آب کم در سطح
کلمات کلیدی
زاویه تماس پایدار نفوذ به نفوذ، جریان ناپایدار، انگشت کوچک، دفع آب
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی

SummaryDespite growing knowledge about water repellent soils it is not well investigated how soil water repellency (SWR) of a lower level influences the in situ water infiltration into soils. Hence, we investigated a sandy soil where we found subcritical water repellency and unexpected stable (persistent) contact angles (CAs) in the subsoil characterized by CA measurements in the laboratory. To characterize the influence of this persistence on in situ water infiltration, a ponded tracer infiltration experiment was carried out. During the infiltration, hydraulic sensors revealed a slight saturation at the wetting front which is a sign for unstable flow. The excavated dye-stained infiltration zone was conical and its lateral extent decreased with increasing depth, showing characteristics of a macro-finger. We suggest the subsoil to exhibit a strong hysteretic water retention characteristic governing the infiltration process, but we could not verify this by standard laboratory measurements, as strongly persistent SWR prevented the fast wetting of the soil samples. Close to saturation the persistence of SWR led to a wetting period of soil samples of at least 56 days to overcome SWR and reaching an equilibrium state. There are three major conclusions of this study: 1. In contrast to many other studies we found persistent SWR also in the subsoil and not only in the humic topsoil, 2. The shape of the wetting front is contrary to common expectations for homogeneous sandy soils and 3. The wettability characteristics found might also be relevant for assessing infiltration dynamics at other sites regarding the fact that those observations are not obvious.

► In a sandy soil the persistence of water repellency increases with depth. ► Stable contact angles in the subsoil were determined in the laboratory. ► Ponded infiltration showed slight saturation overshoot indicating unstable flow. ► The excavated tracer pattern was conical shaped. ► The persistent water repellency triggered the non-ideal dye pattern.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Hydrology - Volume 484, 25 March 2013, Pages 45-54
نویسندگان
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