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1)  soil in alluvial plain by the Yellow River
黄泛平原土壤
1.
On the coincidence between the Square Diagram of the Fu Xi s 64 hexagrams and the sectional drawing of the soil in alluvial plain by the Yellow River;
论《伏羲六十四卦方图》与黄泛平原土壤剖面之契合
2)  flood-plain soil
[农]泛滥平原土壤
3)  Yellow River floodplain
黄泛平原
1.
Based on the analysis of wind-sand disaster control and shelter belt status of the wind-sand impacted region in Yellow River floodplain in Shandong province,it was considered that the shelter system is single and defending capacity is weak,and the wind-sand movement of surface is still strong.
在分析山东省黄泛平原风沙灾害治理及防护林体系现状的基础上,指出黄泛平原风沙区防护体系单一,防护能力薄弱,近地表风沙活动强烈;黄泛平原是山东省的畜牧业发展主要区域,但其天然草地资源不足,发展潜力有限;土壤质地差、肥力低,风、沙、薄成为制约黄泛平原风沙区农牧业发展的障碍因子,但黄泛平原光热资源丰富,水分资源充足,适宜于种植牧草。
2.
Algonquin,Astragalus adsurgens,Melilotus suaveolens in wind-sandy land of Yellow River floodplain were studied by field testing and indoor analysis.
通过野外取样与室内分析相结合的方法,研究了黄泛平原风沙化土地种植高丹草、无芒雀麦、黑麦草、阿尔冈金苜蓿、沙打旺、草木樨后的土壤改良效果。
4)  Yellow River flood plain
黄泛平原
1.
Study on relationship of soil nutrients and various particlesin fluvo-aquic soils on the Yellow River flood plain,north China;
华北黄泛平原潮土土壤养分与土壤粒级的关系研究
2.
Research on the Relationship between Particles and Levels of Phosphorus in the Alluvial Soils on the Yellow River Flood Plain in North China;
华北黄泛平原潮土磷素含量与土壤粒级的关系研究
3.
A Study on Modes of Agro-forestry Management in Yellow River Flood Plain(Huangfan Plain);
黄泛平原林农复合经营模式的探讨
5)  Huangfan Plain
黄泛平原
1.
Study on Field Water Dynamic of Coarse Sandy Soil in Huangfan Plain;
黄泛平原粗砂潮土农田土壤水分动态研究
2.
The Study of the Stability of Agriculture in Huangfan Plain in Qianlong Period of Qing Dynasty;
乾隆时期黄泛平原农业生产稳定性研究
3.
Through the determination of water characteristic curve, specific water volume, moisture constant,permeation coefficient, the situation of pore space and other physical characteristics of sandy soil in Huangfan plain, it was found that the empirical equation θ=AS -B could well simulate the water characteristic curve of soil during the low and medium suction (0.
通过对黄泛平原砂质潮土水分特征曲线、比水容量、水分常数、渗透系数、孔隙状况及部分物理性质的测定,发现经验方程θ= AS- B在低、中吸力段(0。
6)  Plain reservoirs in Yellow Riverflooded area
黄泛区平原水库
补充资料:黄淮平原
黄淮平原

    位于中国河南省东部、山东省西部黄河以南及安徽省、江苏省淮河以北。是华北平原的南部。主要由黄河、淮河下游泥沙冲积而成。地形平坦,仅徐州地区略见小丘。西部和南部山麓平原,海拔大多在80米左右;中部平原,海拔多在35~80米之间;东部滨海一带,海拔仅2~3米。平原中多低洼区,湖泊众多,分布在淮河中下游一带。山东丘陵的西部和南部边缘,有著名的京杭运河将这些湖泊沟通,成为中国南北水路交通要道。历史上黄河在平原上多次泛滥改道,从兰考经商丘、徐州到淮阴的黄河故道两侧多沙地、沙丘,面积6000平方千米。1949年后,在淮河上游已建成大中小水库近5000座;在中游利用湖洼地修建蓄洪滞洪工程;下游开辟入海入江通道。现平原上河渠纵横,涵闸密布,稻麦两熟。产小麦、杂粮、棉花,为中国重要农业区。
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