1) oblique fine soil plain
倾斜细土平原
1.
Analysis of the distribution regularity and the salinized soil expansion action of salinized soil in oblique fine soil plain;
倾斜细土平原盐渍土分布规律及盐胀作用分析
2) inclined plain
倾斜平原
3) piedmont sloping plain
山前倾斜平原
1.
The formation of the chemical composition of the Quaternary loose deposited underground porous water system of the Fukang-zhundong piedmont sloping plain at Tianshan north foot is chiefly influenced by the hydro-chemical properties of the recharge water resource (melted ice-snow wter , rather highly mineralized surface floodwater in rocky mountainous area).
天山北麓阜康—准东山前倾斜平原第四纪松散堆积地下孔隙水含水系统水化学成分形成，主要受补给水源（冰雪融水，基岩山区较高矿化地表洪水）水化学性质影响，水中离子含量比例关系受矿化度影响明显，含水系统水循环交替迅速使排泄区中等矿化水淡化，地下水中Ｓｒ含量较高，普遍达到饮用矿泉水指标。
4) fine soil plain area
细土平原区
1.
On the basis of analyzing the hydrogeological conditions of fine soil plain area in Xinjiang, the process of migration and accumulation of the salt in phreatic water under different drainage circumstances is expounded, thus the effective measures of shaft drainage and irrigation to improve the salinization of soil and prevent soil resalinization are propose
该文通过对新疆细土平原区水文地质条件的分析 ,论述了潜水在不同排泄条件下水中盐分的运移和积聚的过程 ,从而提出竖井排灌是改良土壤盐渍化、防止土壤返盐的有效措
5) tiltedfill
填土倾斜
6) original dip
原生倾斜
补充资料：土默川平原
因明清时代为蒙古族土默特部居住地而得名。又称前套平原或呼和浩特平原。位于自治区中南部。西起包头市郊区东乌不拉沟口，东至蛮汉山，北靠大青山，南濒黄河及和林格尔黄土丘陵。东西长约330公里，南北窄，西部平均宽19公里，东部宽达200多公里总面积约1万平方公里，系由黄河及其支流大黑河冲积而成。地势西、北、东三面向南倾斜，海拔1000米左右，最低处在黄河沿岸一带。整个平原地势平坦，气候条件适宜，土壤肥沃，水源丰富，盛产小麦、玉米、甜菜、胡麻等作物和各类蔬菜，是内蒙古的“米粮川”。个别地方因排水不畅，地下水位升高，土壤发生盐碱化。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条