1) Sikeshu River
四棵树河
1.
Runoff volume of Sikeshu River and its influential factors of climate;
四棵树河径流量与气候影响因子分析
2.
Analysis of ice-flood in Sikeshu River basin on the north slope of Xinjiang Tianshan mountain;
新疆天山北坡四棵树河冰洪分析
3.
Changing Characteristics of the Meltwater Runoff in the Sikeshu River and Their Potential Influence to the River Runoff
天山四棵树河冰川径流变化特征及其对河流径流的可能影响
2) Sikeshu Sag
四棵树凹陷
1.
Comprehensive Analysis of Hydrocarbon Accumulation in the Southern Margin of Sikeshu Sag in Junggar Basin
准噶尔盆地南缘四棵树凹陷油气成藏综合分析
2.
The dark mudstone of Neogene System in Sikeshu Sag of Junggar Basin is a potential source rock with vitrinite reflectance(Ro)of 0.
准噶尔盆地四棵树凹陷新近系暗色泥岩镜质体反射率Ro为0。
3) Sikeshu Section
四棵树剖面
1.
The Sikeshu Section is located on the south-western margin of the Junggar Basin, Xinjiang, and about 40 km southwest of Wusu city.
在实测四棵树剖面的基础上,详细研究了其孢粉组合特征,建立了5个孢粉组合:1)Cameratitriletes和Zonotriletes-Protopinus-Cycadopites组合,2)Cyatheaceae-Pinaceae-Cycadopites组合,3)Cyatheaceae-Pinaceae-Quadraeculina-Cycadopites组合,4)Cyatheaceae-Quadraeculina-Piceaepollenites组合和5)Cyatheaceae-Clas-sopollis-Pinaceae组合,分别产于上三叠统的小泉沟群、下侏罗统的八道湾组和三工河组、中侏罗统的西山窑组和头屯河组。
4) The tree is four feet around.
这棵树周长四尺。
6) single trees
单棵树
1.
By considering the effects of weather and background as well as the structure of trees,a 3 D model for calculating the transient temperature field of single trees was established by using the principle of heat transfer.
综合考虑自然气象条件和背景环境及树木自身结构的影响 ,运用传热学原理 ,建立了单棵树三维瞬态温度场计算模型 。
补充资料：永宁四棵树
永宁四棵树
四棵树在宁夏永宁县李俊镇郭家湾子村北，有四棵粗细基本相同的古老银白杨，树高约21米，直径为1米，四棵树呈正方形布局，树与树之间相距8米，树冠遮地面积约1亩左右。按古树的年轮推算，约有320年或370年历史。
四棵树虽经风雨300余年，仍然苍劲挺拔，古树新枝，繁茂异常，枝头上栖息着已经少见的珍禽"苍鹭"，其鸣声闻于数里之外，当地流传着种种关于四棵树的传说，更使古树增添了一种神秘的色彩。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。