API PUBL 4527-1993 Evaluation of Limiting Constituents Suggested for Land Disposal of Exploration and Production Wastes《评价体现石油勘探生产废弃物陆地扩散的极限成分》.pdf
《API PUBL 4527-1993 Evaluation of Limiting Constituents Suggested for Land Disposal of Exploration and Production Wastes《评价体现石油勘探生产废弃物陆地扩散的极限成分》.pdf》由会员分享,可在线阅读,更多相关《API PUBL 4527-1993 Evaluation of Limiting Constituents Suggested for Land Disposal of Exploration and Production Wastes《评价体现石油勘探生产废弃物陆地扩散的极限成分》.pdf(67页珍藏版)》请在麦多课文档分享上搜索。
1、API PUBLS4527 93 = 0732290 05LLO2 556 = Evaluation of Limiting Constituents Suggested for Land Disposal of Exploration and Production Wastes HEALTH AND ENVIRONMENTAL SCIENCES DEPARTMENT AND EXPLORATION AND PRODUCTION DEPARTMENT API PUBLICATION NUMBER 4527 AUGUST 1993 American Petroleum Institute 122
2、0 L Street. Northwest 111 Washington, D.C. 20005 API PUBLJ4527 93 0732290 0517103 492 Eva1 uation of Li miti ng Constituents Suggested for Land Disposal of Exploration and Production Wastes Health and Environmental Sciences Department and Exploration and Production Department API PUBLICATION NUMBER
3、4527 PREPARED UNDER CONTRACT BY: LLOYD E. DEUEL, JR., Ph.D. SOIL ANALYTICAL SERVICES, INC. 41 5 GRAHAM ROAD COLLEGE STATION, TEXAS 77485 JULY 1991 Amerlcan Petroleum Institute API PUBL*4527 93 0732290 0517104 329 FOREWORD API PUBLICATIONS NECESSARILY ADDRESS PROBLEMS OF A GENERAL NATURE. WITH RESPEC
4、T TO PARTICULAR CIRCUMSTANCES, LOCAL, STATE, AND FEDERAL LAWS AND REGULATIONS SHOULD BE REVIEWED. AFI IS NOT UNDERTmG TO MEET THE DUTIES OF EMPLOYERS, MANUFAC- TURERS, OR SUPPLIERS To WARN AND PROPERLY TRAIN AND EQUIP THEIR EMPLOYEES, AND OTHERS EXPOSED, CONCERNING HEALTH AND SAFETY RISKS AND PRECAU
5、TIONS, NOR UNDFRTAKING THEIR OBLIGATIONS UNDER LOCAL, STATE, OR FEDERAL LAWS. NOTHING CONTAINED IN ANY API PUBLICATION IS TO BE CONSTRUED AS GRANTING ANY RIGHT, BY IMPLICATION OR OTHERWISE, FOR THE MANU- FA-, SALE, OR USE OF ANY METHOD, APPARATUS, OR PRODUCT COV- ERED BY LETTERS PATENT. NEITHER SHOU
6、LD ANYTHING CONTAINED IN ITY FOR INFRINGEMENT OF LETERS PATENT. THE PUBLICATION BE CONSTRUED AS INSURING ANYONE AGAINST LIABIL- Cbpy-right (u 1993 American Petroieum Institute ii API PUBL*4527 33 = 0732230 0537305 265 Section 1: Section 2: TABLE OF CONTENTS Page Introduction and Executive Summary 1
7、Technical Justification and Literature Review 3 2.1 Limiting Constituents 3 2.2 Salinity . 3 2.3 Sodicity (ESP and SAR) 14 2.4 Hydrocarbons . 17 2.5 Summary . 24 Section 3: Pit Operations and Land Disposal . 25 3.1 Pit Operations 25 3.2 Summary of Guideline Thresholds and Application . 29 3.3 Flow D
8、iagram for Pit Liquid Disposal . 31 3.4 Flow Diagram for Pit Solids Disposal . 32 3.5 Parameters and Example Calculations for Management of Pit Wastes by Land Treatment 34 References . 39 Appendix 47 API PUBLX4527 93 W 0732290 0517106 LTL W SECTION 1 INTRODUCTION AND EXECUTIVE SUMMARY Onshore explor
9、ation and production (E and oil and grease (O the rationale being that salt accumulated outside the bulk soil mass (in pores and on ped surfaces) is more easily displaced than that penetrated into and reacted with the bulk soil mass. If the salinity is initially too high for a given crop after land
10、applications of waste, soils will generally recover following rainfall or irrigation containing less salt because excess salts are leached when adequate drainage is present. Growth of more salt tolerant plants may be desirable during the interim 7 API PUBLX4527 93 0732290 05LLL3 331 cn n. O L - a o
11、a, a Co .- n L a, a LL .- .- U a m O L m c O o L c O O +., ci o (d a, Q 3 O o X a LL - ci 3 C Ca a, e r U U a n a, O - .- a E 3 c o, O cn L o m Lo cv O cv Lo F O r Lo O - Y 8 API PUBLX4527 93 0732290 0517115 LO4 cn Q O L a, 0 U S cd cn a, Co cn cd t nn aia ao a o 6 3 o a a lL o) E CLL O c9 Lo cv O C
12、u In 7 O 7 Lo O h L IL 9 API PUBL*4527 93 0732290 05L7LLb 040 W Lo c7 o Cll Lo N O N lo Y O Y Lo O h CD a3 -# x Q)= O U a.+) 10 API PUBLa4527 93 0732290 0517117 T87 between application and recovery (Foth and Turk, 1972). Reclama- tion of salt-containing soils may be hastened through the appli- catio
13、n of calcium sulfate (gypsum) which results in the replacement of exchangeable sodium by calcium (Oster and Rhoades, 1984). Plants grown on gypsiferous soils will tolerate an EC approximately 2 mmho/cm higher than those shown in Figures 1 through 3 (Mass, 1986). This is because gypsum is dissolved a
14、t moisture equivalents used in preparing saturated soil extracts for analysis but not at moisture equivalents normal to field conditions. USDA Handbook 60 (U.S. Salinity Laboratory Staff,1954) clas- sifies water with EC values above 2.25 mmho/cm as unfit for agricultural purposes except under very s
15、pecial circumstances. Soils with salinity levels 4 mmho/cm are considered saline. The recommended criteria of 4 mmho/cm is too high for the mo:re salt sensitive crops (Table i), and some adjustments may have to be made relative to intended land use. Miller and Pesaran (:L980) found that high concent
16、rations of soluble salts in mud-treated soil hindered plant growth in a 1:l mud:soil mixture. their data where EC of the mud:soil mixture was 200 mmho/cm) posed a threat to local- ized groundwater resources. However, the EC of 200 mmho/cm greatly exceeds the recommended threshold of 4 mmho/cm. Bates
17、 (1988), working with a freshwater drilling fluid, demon- strated that C1 was not retained in the zone of incorporation when mixed with surface soil. The criteria of 4 mmho/cm (2452 mg/liter TDS for riA1r = 613) can be expected to have no measurable impact on groundwater even in the most sensitive h
18、ydrological settings. Water and associat- ed dissolved constituents do not move through soils as an isolat- ed unit (plug flow), instead there is a natural redistribution controlled by water potentials, pore dynamics, dispersion, and 12 API PUBL*12) in soil solution cause Ca and Mg deficiencies in p
19、lants by both antagonistic reactions and shift- ing of solubilities by common ion effect (Kramer, 1969; U.S. Salinity Laboratory Staff, 1954). 15 API PUBLx4527 93 = 0732290 0517122 344 = Soils reacted with solutions of high SAR are at risk of becoming sodic. A soil is termed sodic when the ESP excee
20、ds 15% of the CEC (U.S. Salinity Laboratory Staff, 1954). The most distinguishing feature of sodic soils is their lack of structure and tendency to disperse in water. A dispersed soil condition has a devastating impact on plants by limiting the free exchange of air and infiltration of water (Reeve a
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