間層片麻巖 的英文怎麼說

中文拼音 [jiāncéngpiānyán]
間層片麻巖 英文
lit par lit gneiss
  • : 間Ⅰ名詞1 (中間) between; among 2 (一定的空間或時間里) with a definite time or space 3 (一間...
  • : i 量詞1 (用於重疊、積累的東西 如樓層、階層、地層) storey; tier; stratum 2 (用於可以分項分步的...
  • : 片構詞成分。
  • : 麻構詞成分。
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  1. When the rainfall intensity is steady, the time longer of rainfall is, the thinner of slope soil is, the more water in slope soil before rain is, the easier the water flows on the ground. 2

    因此,在太行山區,在一定的降雨強度下,降雨時越長,坡面土壤越薄,坡面土壤雨前的含水量越高,越容易形成地表徑流。
  2. And we have got the following result : 1. the technique of storing water in soil in gneiss area of tai - hang mountain : the more water in soil before rain is, the less water capability of soil is, the time shorter of water flowing from soil is, the easier the water flows on the ground ; the soil capability of reserving water of different soil thickness is terrace > acacia land > pine land > grass land, so the soil is more thick, the soil capacity which contains water is more large ; the accumulated water that flows on the ground is remarkable related with the logarithms of rain time

    太行山區土壤蓄水規律:雨前土壤含水量越高,土壤可蓄水量越小,出流所需時越短,容易形成地表徑流;不同土厚度的土壤蓄水量為:梯田刺槐林地油松林地草地;累積地表徑流量與降雨時的對數呈顯著正相關,擬合方程為w = a + blnt ,相關系數均大於0 . 92 ,即在降雨強度一定的前提下,降雨時越長,累計地表徑流量越多。
  3. After rain, the soil water content is higher, while no rain, the soil water content decreases faster relatively. in autumn, the soil water content begins to drop, but the drop range is small than summer. during continual d rought, the soil water content of surface layer approaches to that of middle layer and under layer ; water conservation measures can increase chestnut ' s new branch remarkably, results difference among water conservation measures are not significant, meanwhile, water cons

    而在持續乾旱期,表土壤的含水量接近於中下土壤的含水量;保水措施能使新梢明顯增長,而保水措施之的效果差異不明顯;同時保水措施並不能使新梢直徑明顯增粗;保水措施對成齡板栗樹根莖地徑的增粗生長影響不大;綜合以上試驗結果,秸稈覆蓋為太行山區的最佳的保水措施,地膜覆蓋其次。
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