1) dry highland of Loess Plateau
黄土旱塬
1.
Adaptability of Hybrid-Maize model and potential productivity estimation of spring maize on dry highland of loess plateau;
黄土旱塬Hybrid-Maize模型适应性及春玉米生产潜力估算
2.
A long term experiment in dry highland of Loess Plateau was conducted,the results show that serious nitrate accumulation would be found in soil deep profile in long term overuse or unbalance application of nitrogen.
在黄土旱塬长期定位测定结果表明 ,长期过量或不平衡使用氮肥将导致硝态氮在土壤深层的严重积累。
3) loess tableland
黄土塬
1.
Application of 3D seismic survey in loess tableland;
黄土塬山地三维地震勘探应用实例
2.
Application of tomostatics in data processing from crooked wide line geometry in Loess Tableland.;
层析静校正在黄土塬弯宽线资料处理中的应用
3.
Seismic acquisition with a swath of lines in area of loess tableland;
鄂尔多斯盆地黄土塬区多线地震采集技术
4) loess tableland area
黄土塬区
1.
Effects of land use type and slope position on soil physical properties in loess tableland area.;
黄土塬区不同地形部位和土地利用方式对土壤物理性质的影响
5) Loess plateau
黄土塬区
1.
The seasonal variation of CO_2 flux in a wheat field of the Loess Plateau;
黄土塬区麦田CO_2通量季节变化
2.
Evaluation of CLIGEN precipitation elements on Loess Plateau;
CLIGEN降水要素在黄土塬区的适应性评估
6) loess platform
黄土台塬
1.
Landslide induced by over-irrigation in loess platform areas in Gansu Province;
甘肃黄土台塬区农业过量灌溉引起的滑坡灾害
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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