1) snowmelt erosion
融雪侵蚀
1.
So it is necessary to predict the snowmelt erosion in these areas, which should include the generation of snowmelt runoff, the soil loss it causes, the changes in soil pr.
因此在这些地区进行融雪侵蚀预报十分必要,它主要包括融雪径流的产生,及其形成的土壤侵蚀量,冻融过程导致土壤性状的变化,以及由此造成的对土壤可蚀性的影响。
2) snowmelt-runoff erosivity
融雪径流侵蚀力
1.
For predicting soil erosion by models,it is necessary to quantify snowmelt-runoff erosivity(RW) and rainfall erosivity(R) separately.
东北地区融雪侵蚀十分显著,进行土壤侵蚀预报时,需要计算降雨侵蚀力,也要求推算融雪径流侵蚀力。
3) freeze-thaw erosion
冻融侵蚀
1.
Comparison and analysis of climate environmental variation in two main freeze-thaw erosion regions in China;
我国两大冻融侵蚀区气候环境变化对比分析
2.
Impact of climate change on freeze-thaw function and freeze-thaw erosion in black soil region of Northeast China
气候变化对东北黑土冻融作用与冻融侵蚀发生的影响分析
3.
the hydraulic erosion, the wind erosion, and the freeze-thaw erosion, which account for 6%, 5%, and 89% of the total area of soil erosion, respectively.
分析了西藏地区的水土流失特点和成因,指出西藏地区的土壤侵蚀类型主要有水力侵蚀、风力侵蚀和冻融侵蚀3种类型,水蚀范围较小,约占总侵蚀面积的6%,风蚀范围更小,约占总侵蚀面积的5%,冻融侵蚀面积约占总侵蚀面积的89%,是土壤侵蚀的主要类型;土壤侵蚀类型在地域上成多样化分布,土壤侵蚀在垂直方向上呈规律分布。
5) freezing-thaw erosion area
冻融侵蚀区
1.
By analyzing the distribution of freezing-thaw erosion area,this paper pointed out any characters of freezing-thaw erosion area in Tibet as follows:1) The .
冻融侵蚀区的界定是目前青藏高原冻融侵蚀研究需要解决的重要课题之一。
6) freeze-thaw and weathering erosion
冻融风化侵蚀
补充资料：融雪洪水预报(见冰情预报)
融雪洪水预报(见冰情预报)
rongxue hongshu，融曾洪水预报yubao 见冰情预报。
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