An evaluation of the Olsen test as a measure of plant-available phosphorus in grassland soils derived from basalt parent material

Abstract. Anecdotal and circumstantial evidence have suggested that the Olsen test underestimates plant-available phosphorus (P) in basaltic soils in Northern Ireland. Therefore, the ability of this test to predict plant-available P in basaltic (and non-basaltic) soils was investigated by regressing Olsen-P data against herbage P indices calculated from plant tissue test data using the diagnosis and recommendation integrated system. The average Olsen-P concentration for a range of fields situated on basaltic soils was considerably lower than the average Olsen-P concentration for a range of fields situated on non-basaltic soils, and yet mean sward P status, as given by the herbage P indices, was similar for both groups of fields. Herbage P indices were also much better correlated with Olsen-P measurements in non-basaltic soils than in basaltic soils. Furthermore, at low Olsen-P values (≶9mgPL⁻¹) some swards on basaltic soils were genuinely deficient in P, while others were sufficient or even in surplus for this nutrient. The results confirm that Olsen-P is inadequate as a predictor of plant-available P in basaltic soils. It is concluded that an alternative soil test is needed to provide a reliable assessment of plant-available P in basaltic soils, to prevent overuse of fertilizer and manure P and to minimize the amounts of P entering local watercourses.     

Evaluation of two N cycle models for the prediction of N mineralization from grassland soils in the UK

Abstract. The ability of two nitrogen cycle models, of contrasting complexity, to predict N mineralization from a range of grassland soils in the UK, was evaluated. These were NCYCLE, a simple mass balance model of the N cycle in UK grasslands, and CENTURY, a more complex model simulating long-term C, N, P & S dynamics in grassland ecosystems. The models were tested using field measurements of net N mineralization from a range of grassland soils (differing in soil type, history & management practice), obtained over a 2 year period using a soil core incubation technique. This method was considered to measure the total net release of mineral N from the soil organic matter over a specified time, including N which may have been recycled several times. NCYCLE consistently under-estimated mineralization rates at all sites. By contrast, there was some correlation between CENTURY predictions of net N mineralization and field measurements. This may have reflected the different abilities of the two models to simulate N recycling. Neither model, however, was able to predict adequately the effect of cultivation and reseeding on net N mineralization.     

宁南山区旱地紫花苜蓿土壤水分及产量动态研究

对宁南山区旱地紫花苜蓿土壤水分及产量动态进行了研究。结果表明,随苜蓿草龄的延长,土壤深层水分亏缺严重草地底层与中层对表层水分具有明显的补偿作用;伏秋降对水冬前土壤蓄水亦有重要作用;产量随草延长呈中间高两头低的态热,６－８年以后草地须及时更新。     

甘肃省草地植物区系研究

按照吴征镒的中国种子植物分布区划分,对甘肃省草地植物区系的组成、植物科、属的统计及其分布特征进行了分析,得出甘肃省草地植物区系物种丰富,共有植物154科706属2 128种;地理成分温带性质明显;有一定的过渡性及相互渗透的特点;区系成分以年轻成分为主,中国特有属较少。     

云南省岩溶地区石漠化草原现状及分区保护与修复策略

据最新调查数据,云南省石漠化草原主要分布于曲靖、昆明、红河等5个州( 市),总面积 37.97 万hm²,占岩溶土地面积的3.53%,其分布最广的海拔区间为1 500~2 500 m,占比47.85%, 基岩裸露度分布区间为30%~94%,以植被盖度为10%~19%的分布区间面积最广,占比37.85%, 绝大部分分布于土层薄甚至极薄区域,占比达92.10%。根据石漠化草原空间分布特征,在充分衔 接各大生态保护和修复工程建设规划基础上,统筹考虑岩溶生态系统的完整性、地理单元的连续性 和经济社会发展的可持续性,将云南省石漠化草原区划为6个分区,分区阐述石漠化草原生态保护 与修复策略。     

论森林与草原的作用

本文在文献综述和个人实践的基础上,对森林生态系统和草原生态系统作了描述,分析了它们的特色和功能,评价了林业和草业在西部大开发中的相互关系。     

基于GIS的藏东横断山区土壤侵蚀分布特征研究

利用ARC/INFO的空间分析与统计分析功能,从海拔、坡度、土壤以及土地利用四个方面,对藏东横断山区土壤侵蚀的空间分布特征进行了研究。结果表明:(1)从总体上来讲,三江河谷地带水蚀较强;山体中部以微度侵蚀为主,而森林采伐迹地土壤侵蚀严重;海拔4500m以上地带,冻融侵蚀严重。(2)不同的海拔与坡度等级下,4000-5000m与25°-35°土壤侵蚀最强。(3)水力侵蚀主要发生在褐土与灰褐土土壤类型,冻融侵蚀主要发生在寒冻土、黑毡土以及草毡土土壤类型。(4)土壤侵蚀主要发生在草地和林地,低覆盖草地上冻融侵蚀尤为严重。通过土壤侵蚀分布特征的研究,为土壤侵蚀防治对策提供科学依据。     

分布型过牧:一个被忽视的内蒙古草原退化的原因

过牧已成为学界和决策部门普遍认可的草原退化原因之一。它是基于牲畜总数超过草原承载力这一简单逻辑来定义的。为了消除过牧,中国采取许多措施以降低牲畜数量和增加草料产量。但是,草原"整体恶化"的局面并没有改变。通过案例调查研究村一级的草原管理和牲畜分布方式,本文提出除了目前单纯强调牲畜总量的解释("数量型过牧")外,由于产权制度变化引起的牲畜分布变化也是导致草原退化的重要原因,本文将其定义为"分布型过牧"。