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1)  Beiyuan
北塬
1.
Climate Instability Revealed in the Beiyuan CaCO_3 Record during the Last Interglacial Age;
北塬剖面碳酸钙记录的末次间冰期气候不稳定性
2)  Weibei Upland
渭北旱塬
1.
Effect of Apple Base on Regional Water Cycle in Weibei Upland of the Loess Plateau;
黄土区渭北旱塬苹果基地对区域水循环的影响
2.
Research on Growing Grass in Apple Orchard in Weibei Upland;
渭北旱塬苹果园的生草效应
3.
The experiment was held in an apple orchard located in Weibei upland without irrigation system.
试验设在无灌溉条件的渭北旱塬苹果园,试验园为1992年春栽植的矮化中间砧富士果园,品种长富2号,中间砧M_(26),基砧新疆野苹果,株行距为2×3。
3)  Weibei Loess Upland
渭北台塬
1.
Characteristics Analysis of Landslip Group in the Weibei Loess Upland;
渭北台塬滑坡带特征分析
4)  Weibei Rainfed Highland
渭北旱塬
1.
Studies on photosynthetic characteristics of Vitis vinifera L.cv.Cabernet sauvignon during berry expansion period in Weibei Rainfed Highland;
渭北旱塬‘赤霞珠’葡萄浆果膨大期光合特性研究
2.
Research on Winter wheat Fertilizer Practiceunder Different Annual Precipitations on Weibei Rainfed Highland;
渭北旱塬不同降水年型冬小麦施肥技术的研究
3.
Practice and Reflections on Agricultural Industrial Structure Adjustment in Weibei Rainfed Highland;
渭北旱塬农业产业结构调整的实践与思考——以彬县为例
5)  Weibei dryland
渭北旱塬
1.
Mineral N accumulation and distribution of apple orchard soil on the Weibei dryland;
渭北旱塬苹果园土壤矿质氮累积与分布研究
2.
Analysis on characteristics and influencing factors of soil nitrogen for terrace in the Weibei dryland;
渭北旱塬梯田土壤氮素特征及影响因素分析
3.
The characteristic,variability in 80 cm profile of soil potassium and its influencing factors in terrace were studied systematically in the Weibei dryland.
对渭北旱塬梯田土壤钾素特征、剖面变异性及影响因素的系统研究表明,表层各形态钾素中有效性钾和速效钾的空间变异性最大,钾素分布并不平衡;整体来看,因富钾矿物的作用导致钾储量(矿物钾和全钾)充盈,但约95%对植物长期无效;有效钾素(有效性钾和速效钾)的供应及潜在给源(缓效钾)都较富足。
6)  Weibei Plateau
渭北旱塬
1.
Study on Effects of Agricultural Measures on Growth and Yield of Maize in Drylands of Weibei Plateau of Shaanxi Province
农艺措施和施肥对渭北旱塬旱地玉米的影响
2.
Yongshou town is located Weibei Plateau of hilly and gully region,is typically a major agricultural town in the level of economic development in underdeveloped areas belonging.
永寿县豆家镇位于渭北旱塬丘陵沟壑区,属于典型的农业大镇,在经济发展水平上属于欠发达地区。
补充资料:董志塬
董志塬

    位于中国甘肃省东部。汉代称彭池塬,简称彭塬。北起驿马关至庆阳城一线,南止泾河谷地,东西介于马连河和蒲河间。包括甘肃省庆阳县大部及宁县、合水县各一部分。南北长87千米,东西宽36千米左右。面积2260平方千米。为陇东面积最大而较平坦完整的黄土塬。塬面海拔1200~1450米。有13条较大河沟呈辐辏状向塬心伸入,分割塬面成多数碎块。一般沟壑深150~200米。大小沟壑占面积的61%,荒坡又占沟壑面积57%。塬面年降水量约在500毫米左右,年均温8~10℃,无霜期150~180天。为冬小麦主产区。
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