1)  paleochannel
古水道
2)  Ancient paddy soil
古水稻土
1.
Soil samples of current paddy soils,ancient paddy soil/ancient dry land soil,and bottom soils were collected from two sites in Chuodunshan Site of Majiabang Culture(about 6 000a).
kg-1,主要来源于大气沉降;古水稻土中PAHs含量明显降低,仅为56。
2.
Previous studies suggested that two layers of ancient paddy soils existed in Holocene strata at the lower Changjiang River delta region in China,but little evidence of soil chemical and physical data has been offered up to now.
前人研究认为,在长江下游地区绰墩农业遗址的全新世地层中存在2个古水稻土层,但到目前为止尚缺乏土壤化学和物理学方面的证据。
3)  paleocurrent
古水流
1.
The principle and application of magnetic fabric to paleocurrent estimation of drilling cores;
岩心磁组构分析古水流方向的原理与应用
2.
A geometrical method of calculating paleocurrent direction using seismic progradation reflection characteristics;
利用地震前积反射特征确定古水流方向的沉积几何方法
3.
In order to confirm the sedimentary source direction of Yanchang Formation in Yichuan area of Ordos Basin,according as abundant analysis and test data,using characteristic of the sandstone lithology,the features of light and heavy mineral group,paleocurrent direction,and rare earth element distributing pattern,anal.
依据大量分析化验数据,根据砂岩岩石学特征、轻重矿物组合特征、古水流方向、碎屑粒度变化及稀土元素分配模式等,对研究区延长组物源进行综合研究。
4)  paleowater depth
古水深
5)  paleo-hydrodynamics
古水动力
1.
Before the characteristics of fluid migration and accumulation being studied, evolution history of paleo-hydrodynamics must be restored first of all, because of being as specific history events set in geologically history periods.
由于油气的运聚与成藏作用都是发生于地质历史时期的特定历史事件 ,要准确分析流体运移特征 ,就必须首先了解古水动力的演化历史。
6)  ancient hydrological network
古水文网
1.
This paper researches the vicissitude and space distribution law of the ancient hydrological network in Sanjiang Plain in the main geology history section.
研究了三江平原各个主要地史时期古水文网的变迁和空间分布规律。
7)  ancient paddy soils
古水稻土
1.
PCR-DGGE analyses of bacterial and archaeal community diversities in ancient paddy soils discovered in Chuodunshan Site, Suzhou, China;
绰墩山遗址古水稻土细菌与古菌群落的PCR-DGGE分析
8)  palaeocurrent
古水流
1.
Analysis on sedimentary provenance and palaeocurrent in Yao I Member in northern Gulong area;
古龙北地区姚一段地层沉积物源及古水流分析
2.
This paper aims to analyze the stratigraphic and petrological characteristics, the palaeocurrent, and the clastic compositions of Xueshan Formation.
本文重点研究了雪山组的地层特征、古水流特征以及砂岩碎屑组分特征,在此基础上简单分析了其沉积相特征。
3.
Based on the direction of palaeocurrent revealed by the oblique beddings in the sand.
本文根据山西组主要砂岩体中斜层理反映的古水流流向、砂岩体成因及厚度特征和沉积相分布资料,论证了登封煤田在早二叠世早期的海岸线形态是在总体NE-SW走向的背景上有一个向NW方向凹进的海湾。
9)  ancient pool
古水池
1.
Widely distributed calcite and aragonite crystal in the cave passage are originated from ancient pool deposits.
洞内大片分布的石花起源于四大古水池沉积物的存在。
10)  paleo water media
古水介质
补充资料:水稻土
水稻土
paday soil

   长期种植水稻形成的具有氧化还原交替特点的耕作土壤。长期植稻引起土壤有机质含量增加,有机质组成趋于简单;饱和土壤中盐基淋溶,不饱和土壤发生复盐基作用;铁、锰元素在土壤中移动,耕层含量较低,淀积层较高,潜育层最低;粘粒矿物发生分解和合成。随着水稻土形成作用的发展,出现水稻土特有的发生层:耕作层、犁底层、淀积或斑纹层、漂洗层、潜育层。水稻土分布极广,凡气候适宜又有水源灌溉的土壤均可经种植水稻而形成。主要分布在北纬35°至南纬23°之间,以亚洲最多。中国集中在长江下游平原、四川盆地、珠江三角洲和台湾西部平原。水稻土的类型主要有:①淹育性水稻土。多分布在丘陵,地下水位低,耕层浅,肥力不高。②潴育性水稻土。分布于冲积平原,地下水位一般60~150厘米,土壤通透性好,矿质养分丰富,肥力高。③潜育性水稻土。分布在丘陵谷地或冲积平原洼地,土质轻粘,有的有泥核,耕作困难,有效养分低,尤磷、钾不足。④漂洗型水稻土。在下降水或侧渗水影响下形成,土层紧实,通透性差,有机质含量低,养分贫乏。高产水稻土应是耕层深厚,犁底层不太紧实,通气透水,质地适中,耕性良好,水渗透快慢适度,养分供应协调。
   
   

水稻土剖面

水稻土剖面

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