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Soil Physicochemical Properties of Cultivated Land in Different Farming Years in Korqin Sand Land

机译:Korqin沙地不同农业年耕地土壤理化特性

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Chose cultivated land in Naiman County, this article carried on comparative analysis for soil physicochemical properties of cultivated land in different farming years. This included change characteristics of soil physicochemical properties with different farming years in different slope positions (windward slope, sloping top and leeward slope) of cultivated land and quantitative analysis between farming years and soil physicochemical properties. The results showed that: (1) there were different changes in soil texture in different slope positions of cultivated land in different farming years: at first 15 years, in the windward slope, the soil texture emerged good trend year by year, but after 30 years of farming, the soil texture get significantly worse. In the sloping top and leeward slope, the soil texture was changed for the better trend along with the increase of farming years. (2) There were different changes in soil nutrients in different slope positions of cultivated land during different farming years: in the windward slope, farmed from 3 years to 15 years, upward trend showed among the most nutrients and until 30 years, it obviously reduced and drop back to level of the 3 years; There was a rising trend in the leeward part of the nutrients; sloping top was between the middle and more indicators decline in nutrient content than that of increasing. (3) There was relationship between the farming years and soil physicochemical properties: the effects on soil texture was higher than the soil nutrients and correlation between different slope positions was different: in the windward slope, farming years correlated positively with sand and available P and a negative correlation was found between farming years and other indicators. In the sloping top, farming years correlated negatively with sand, total N, total K, alkaline N and available P, correlated positively with other indicators. In the leeward slope, farming years correlated negatively only with sand and total K, correlated positively with all of other indicators. Korqin sand land is portion of Songliao subsidence zone, northern is Da Hinggan Ling Mountain and its hilly region, central is the alluvial plain formed by the Xiliaohe River and its tributaries, and southern is distribution of the Yanshan Mountain and loess hills, and it is one of the most serious desertification areas in arid and semi-arid zones of northern China. In recent years, it showed increasing trend in land degradation under human factors and natural factor together. This was a serious threat to the sustainable development of local agriculture [1,2]. Farmland area decreased in production which effected by sand disasters covered over than 30% of all crop planted area [3]. Therefore, protection situation of cultivated land in the area was serious. Land use and management was the most common, most direct and profound factors in affecting soil changes [4,5]. Farming years was one of the most important properties of affecting soil changes in Korqin sand land with serious sandstorms. Research has revealed that years of reclamation has a certain extent on different layers of soil physicochemical properties in sandy grassland in Korqin sand land. With the increase of time of reclamation, fine particle fraction decreased, the coarse and fine sand content gradually increased, soil bulk density increased, soil porosity decreased and the amount of total nutrients in the soil also turn down in arable layer [6]. Under the impact of policy and population factors, a large number of lumps have been reclaimed into cultivated land. Lump was suitable for reclamation, changes in soil quality in different parts after reclamation has not been concerned. To this end, this article chose lump cultivated land as research object, carried on comparative analysis for change characteristics of soil physicochemical properties among different slope positions of cultivated land along with different farming year.
机译:本文选择了奈曼县的耕地土地,对不同农业多年耕地土壤理化性质的比较分析。这种耕地不同坡度(迎风坡,倾斜顶部和背展坡面不同农业多年的土壤物理化学性质的变化特征及农业多年与土壤理化性质的定量分析。结果表明:(1)在不同农业年份的耕地坡度不同的土壤质地变化不同:在前15年,在迎风边坡,土壤质地逐年出现良好的趋势,但30岁以下多年的农业,土壤纹理明显更糟。在倾斜的顶部和背风坡上,随着农业年的增加,土壤纹理随着更好的趋势而变化。 (2)在不同农业年内耕地不同斜坡位置的土壤营养素变化不同:在迎风边坡,养殖3岁至15年,上升趋势在最多的营养成分中显示,直到30年,显然减少了并丢回3年的水平;营养成分的背风部呈上升趋势;倾斜的顶部是中间,更多的指标在营养含量下降而不是增加的指标。 (3)农业多年与土壤物理化学性质之间存在关系:对土壤质地的影响高于土壤养分,不同坡度位置之间的相关性不同:在迎风坡度,农业多年与砂和可用的田间相关在农业年和其他指标之间发现了负相关。在倾斜的顶部,养殖年与砂,总N,总K,碱性N和可用P相关,与其他指标正相关。在Leeward坡度中,农业年只与沙子和总K负相关,与所有其他指标正相关。 Korqin Sand Land是松辽沉积区的一部分,北方是大望峰岭山及其丘陵地区,中央是由夏洛河及其支流组成的冲积平原,南方是燕山山和黄土山的分布,是干旱地区最严重的荒漠化地区之一,是中国北方半干旱地区。近年来,它表现出在人类因素和自然因素下的土地退化趋势越来越大。这是对地方农业可持续发展的严重威胁[1,2]。农田面积在生产中减少,覆盖于所有作物地区的30%以上的沙子灾害[3]。因此,该地区耕地的保护状况严重。土地使用和管理是影响土壤变化的最常见,最直接和深刻的因素[4,5]。农业年是影响Korqin沙地的土壤变化的最重要属性之一,具有严重的沙尘暴。研究表明,多年的填海综合症在Korqin沙地砂草地上的土壤物理化学特性不同。随着回收时间的增加,细粒分数降低,粗糙和细砂含量逐渐增加,土壤堆积密度增加,土壤孔隙率下降,土壤中总营养量的量也在耕作层下降[6]。在政策和人口因素的影响下,大量的肿块已被涌入耕地。肿块适合回收,填海后不同部位的土壤质量的变化尚未涉及。为此,本文选择了碎片耕地作为研究对象,对土壤物理化学性质变化特征的比较分析,不同农业年的不同坡度。

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