砖红壤 meaning in Chinese
cabook
laterit soil
laterite soil
lateritic soil
latosol
Examples
- Experimental study on water movement of latosol under drip irrigation
滴灌条件下砖红壤水分运动试验研究 - Leaching of no3 - - n with different fertilizer sorts can be divided into three stages : equilibrium , ascending , descending
应用方程iny : = a + blnt可拟合钾肥在砖红壤中120em处的淋失过程。 - The relationship between the accumulation amount of nh4 + - n leaching and the time could be expressed as equation yt1 / 2 = a + bt with fertilizer applied treatment
各氮肥品种在砖红壤中转化形成no牙一n的过程可分为三个阶段:前期平缓阶段、中期上升阶段和后期下降阶段。 - From 1950s ， geographical - genetic classification theory originated from the former soviet union exerted its extreme impact on soil classification of china
在地理发生分类体系中，按生物气候气候条件，热带、亚热带地带性土壤分别为燥红土、红壤、黄壤、赤红壤和砖红壤。 - This climate make latosol usually as acidic , low levels cation exchanges capacity and low lever base cations , high levels of exchange al , with a high potential for leaching of plant nutrients
这种气候条件使砖红壤成为强酸性土壤，阳离子交换量和盐基饱和度低，铝饱和度高，化肥通过淋溶损失过程就更为突出。