標(biāo)題: Titlebook: Applied Soil Physics; Soil Water and Tempe Ronald J. Hanks,Gaylen L. Ashcroft Textbook 19801st edition Springer-Verlag Berlin Heidelberg 19 [打印本頁(yè)] 作者: Lensometer 時(shí)間: 2025-3-21 20:01
書(shū)目名稱(chēng)Applied Soil Physics影響因子(影響力)
作者: bypass 時(shí)間: 2025-3-21 21:02
Fungi and Industrial PollutantsWe are concerned with radiation and the microclimate above the soil because they have such large influences on:作者: Allure 時(shí)間: 2025-3-22 02:27
Effects of Animals Grazing on FungiThe amount of heat flow in soil influences soil temperature. The temperature of the soil is related to the temperature of the air and vice versa. Both soil and air temperatures have profound influences on plant growth.作者: 使害怕 時(shí)間: 2025-3-22 04:39
Water Quantities,We would first like to point out briefly where the soil fits into the hydrologic cycle and indicate the importance of the soil factors. The hydrologic cycle can, in a simple form, be divided into the following parts:作者: 自作多情 時(shí)間: 2025-3-22 12:20 作者: 態(tài)學(xué) 時(shí)間: 2025-3-22 16:26 作者: intertwine 時(shí)間: 2025-3-22 20:00 作者: vocation 時(shí)間: 2025-3-22 21:39
0172-4207 Overview: 978-1-4684-0184-4Series ISSN 0172-4207 作者: llibretto 時(shí)間: 2025-3-23 03:08 作者: 搖擺 時(shí)間: 2025-3-23 08:51
Fungi and Industrial Pollutantsal is plotted as a function of depth, it results in a smooth curve even across the boundary between layers (see Fig. 3.1 A). When water content is plotted as a function of depth, there is normally a sharp discontinuity in the curve at the boundary between layers (see Fig. 3.1 B).作者: 肥料 時(shí)間: 2025-3-23 10:03 作者: Generalize 時(shí)間: 2025-3-23 16:11 作者: Manifest 時(shí)間: 2025-3-23 19:40 作者: 脆弱么 時(shí)間: 2025-3-23 22:38 作者: 展覽 時(shí)間: 2025-3-24 03:07
Springer-Verlag Berlin Heidelberg 1980作者: 音樂(lè)學(xué)者 時(shí)間: 2025-3-24 07:07
Water Potentials,lude that soil water content is not sufficient to specify the entire status of water in soil. Some of the observations that cause us to believe that there is a need to define some other property associated with soil water are:作者: 省略 時(shí)間: 2025-3-24 13:28
Water Flow in Soil,al is plotted as a function of depth, it results in a smooth curve even across the boundary between layers (see Fig. 3.1 A). When water content is plotted as a function of depth, there is normally a sharp discontinuity in the curve at the boundary between layers (see Fig. 3.1 B).作者: 裝勇敢地做 時(shí)間: 2025-3-24 16:10 作者: demote 時(shí)間: 2025-3-24 20:01 作者: 使殘廢 時(shí)間: 2025-3-25 01:56
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